{"meta":{"query_hash":"e04e5c2efc99","filters":{"venue":"Journal of Geophysical Research Solid Earth"},"cohort_total":536,"direct_labels_cover":0,"predictions_cover":536,"exported":536,"export_cap":100000,"truncated":false,"label_status":"direct model label, unvalidated","prediction_status":"machine_predicted_unvalidated (Codex and Gemma teacher distillation)","score_status":"score_only:v0-immature-baseline","snapshot":{"source":"OpenAlex, pinned release, all 482 partitions","release":"2026-06-24","frame_built":"2026-07-12"},"permalink":"https://metacan.xera.ac/q/e04e5c2efc99","api":"https://metacan.xera.ac/api/v1/cohort?venue=Journal+of+Geophysical+Research+Solid+Earth"},"results":[{"id":"W1484667928","doi":"10.1002/jgrb.50306","title":"Triggering cascades and statistical properties of aftershocks","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":83,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Alberta Innovates - Technology Futures","keywords":"Aftershock; Power law; Shock (circulatory); Exponent; Magnitude (astronomy); Geology; Seismology; Statistics; Mathematics; Physics; Astrophysics","score_opus":0.05540136032496293,"score_gpt":0.30271603183948526,"score_spread":0.24731467151452233,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1484667928","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9857202,0.00013199967,0.011887707,0.000053485852,0.000004125283,0.000059950922,0.0007212369,0.00019485473,0.0012264185],"genre_scores_gemma":[0.9972817,0.00006902363,0.0017557896,0.0000058360138,0.0000090303965,0.000021196769,0.0006478125,0.000017532813,0.00019206977],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995555,0.000058323454,0.000042199455,0.00017389531,0.00011005179,0.00005993841],"domain_scores_gemma":[0.9881511,0.0054656607,0.003757303,0.0013456723,0.00086180447,0.00041858104],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018780796,0.000311937,0.00042798094,0.00338844,0.00050433475,0.0015505465,0.0006842747,0.0004865447,0.0021796268],"category_scores_gemma":[0.017366808,0.00033133104,0.000578283,0.0022794888,0.00069039705,0.0011903356,0.0006575499,0.0005392886,0.00025674218],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027780488,0.00008443049,0.8469131,0.00014082777,0.00026104576,0.0006639661,0.0007920479,0.08680063,0.01623914,0.0111676315,0.0010024423,0.03565701],"study_design_scores_gemma":[0.00004526469,0.00013773331,0.71715903,0.000025766876,0.00011213615,0.00047740492,0.0002611424,0.26948372,0.0046120584,0.0068377573,0.00079296675,0.000055018052],"about_ca_topic_score_codex":0.007930439,"about_ca_topic_score_gemma":0.0052840402,"teacher_disagreement_score":0.007930439,"about_ca_system_score_codex":0.0006856253,"about_ca_system_score_gemma":0.00046355618,"threshold_uncertainty_score":0.015768528},"labels":[],"label_agreement":null},{"id":"W1487245719","doi":"10.1002/2013jb010928","title":"Understanding subsidence in the Mississippi Delta region due to sediment, ice, and ocean loading: Insights from geophysical modeling","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":83,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Canada Research Chairs; University of Ottawa","keywords":"Geology; Post-glacial rebound; Subsidence; Lithosphere; Geodetic datum; Sediment; Sea level; Glacial period; Delta; Geomorphology; Geophysics; Geodesy; Seismology; Tectonics; Oceanography","score_opus":0.13282836809698234,"score_gpt":0.3193974769949339,"score_spread":0.18656910889795159,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1487245719","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99600476,0.00008014815,0.0022231636,0.00019077666,0.0000022970726,0.0000062315025,0.00010152761,0.000020590227,0.0013705477],"genre_scores_gemma":[0.99921846,0.000081704144,0.00050055364,0.000013044965,0.0000017507265,0.0000034292077,0.000039220624,0.0000030131332,0.0001388009],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999641,0.000012684256,0.0000027153594,0.0000086849495,0.0000052014493,0.000006572997],"domain_scores_gemma":[0.9998822,0.000056000856,0.000025772051,0.000009528224,0.000015909487,0.000010651999],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020821557,0.00028763348,0.00021221531,0.00038622777,0.00025900782,0.0005905306,0.00034206215,0.00058656215,0.00063676387],"category_scores_gemma":[0.00054733915,0.0002038145,0.00038720676,0.00030978068,0.00033549804,0.00038606027,0.00028587913,0.0002336501,0.00006322492],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000028219923,0.000048397924,0.03590992,0.000026383677,0.000040012896,0.00014286104,0.00007649296,0.9558294,0.0033809824,0.0011465581,0.000117846495,0.0032529107],"study_design_scores_gemma":[0.0000044586877,0.000023635093,0.013192684,0.0000062122926,0.000012155959,0.000023970826,0.00007359884,0.9856339,0.00030795694,0.0005142971,0.00020178425,0.0000053724266],"about_ca_topic_score_codex":0.059164047,"about_ca_topic_score_gemma":0.03310752,"teacher_disagreement_score":0.059164047,"about_ca_system_score_codex":0.00094283425,"about_ca_system_score_gemma":0.0005641416,"threshold_uncertainty_score":0.11763936},"labels":[],"label_agreement":null},{"id":"W1492904818","doi":"10.1002/2015jb011920","title":"Cascadia subducting plate fluids channelled to fore‐arc mantle corner: ETS and silica deposition","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":135,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Subduction; Mantle (geology); Oceanic crust; Mantle wedge; Transition zone; Crust; Convergent boundary; Seismology; Petrology; Volcanic arc; Geochemistry; Tectonics","score_opus":0.07221616726683112,"score_gpt":0.3273406265674197,"score_spread":0.2551244593005886,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1492904818","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99754506,0.0002554699,0.0002017769,0.00007102591,0.0000027104265,0.000001579558,0.00020625797,0.000025878084,0.001690247],"genre_scores_gemma":[0.99928695,0.00007960766,0.00006637679,0.000005457588,0.0000018360125,8.757685e-7,0.000083208324,0.0000037256864,0.00047191262],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999583,0.000002124003,0.0000035470493,0.000018559474,0.00000942176,0.000008070148],"domain_scores_gemma":[0.9998851,0.00001774552,0.000040678362,0.0000063678526,0.000029281311,0.00002078004],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006479233,0.0003026622,0.00017856494,0.0006000243,0.00033553562,0.00041831666,0.00017451405,0.00018317209,0.0025107325],"category_scores_gemma":[0.0002346928,0.00016017501,0.00017035496,0.00035697644,0.00030761343,0.00022702172,0.00046068142,0.00018170374,0.00021671549],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030216624,0.000018762295,0.7186887,0.00019431111,0.00009873048,0.00075144647,0.0005318877,0.0036386251,0.26549715,0.00057050074,0.0002374387,0.009470373],"study_design_scores_gemma":[0.0000025245138,0.00002385401,0.9909474,0.000005083309,0.000016618596,0.000056507124,0.00020683507,0.00089341844,0.0070812376,0.00015168195,0.0006096156,0.0000051029706],"about_ca_topic_score_codex":0.020715933,"about_ca_topic_score_gemma":0.020301217,"teacher_disagreement_score":0.020715933,"about_ca_system_score_codex":0.000656406,"about_ca_system_score_gemma":0.00032960926,"threshold_uncertainty_score":0.041190684},"labels":[],"label_agreement":null},{"id":"W1496021161","doi":"10.1002/2013jb010364","title":"Constructing empirical resolution diagnostics for kriging and minimum curvature gridding","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Soil Geostatistics and Mapping","field":"Environmental Science","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"University of Toronto; National Science Council","keywords":"Kriging; Variogram; Interpolation (computer graphics); Curvature; Computer science; Algorithm; Function (biology); Resolution (logic); Image resolution; Mathematical optimization; Inverse; Mathematics; Artificial intelligence; Machine learning; Image (mathematics); Geometry","score_opus":0.046998682642256095,"score_gpt":0.3694359417431267,"score_spread":0.3224372591008706,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1496021161","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.08714778,0.000088920504,0.91190565,0.000069139234,0.000008293017,0.000030221092,0.000028338367,0.00016520903,0.0005564379],"genre_scores_gemma":[0.6227165,0.00007366545,0.3767794,0.000030177911,0.000009032168,0.00005726068,0.00007268041,0.000051342144,0.00020991899],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99899143,0.0004892859,0.00005991927,0.000115833405,0.00027728805,0.000066288856],"domain_scores_gemma":[0.99387205,0.0036766408,0.0009298712,0.000673769,0.00073852646,0.00010924211],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0033354468,0.00034889337,0.0003731503,0.001220933,0.00025048488,0.0007172853,0.0005858481,0.00066634914,0.0004396384],"category_scores_gemma":[0.024382755,0.00032621957,0.00043605457,0.00084252714,0.00087711005,0.0011982385,0.0009794137,0.0007827116,0.00009215861],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016675182,0.000057195623,0.01841423,0.0001342814,0.00004864552,0.00021914496,0.00039056773,0.7044206,0.01391792,0.12371473,0.00057840644,0.13793756],"study_design_scores_gemma":[0.0000049982546,0.00002353117,0.0016650739,0.000009270099,0.0000036949168,0.000024735216,0.000016564238,0.98932487,0.0021318658,0.006438202,0.0003471348,0.000010088042],"about_ca_topic_score_codex":0.0021480925,"about_ca_topic_score_gemma":0.0016044046,"teacher_disagreement_score":0.0033354468,"about_ca_system_score_codex":0.00074085715,"about_ca_system_score_gemma":0.0008644538,"threshold_uncertainty_score":0.017639756},"labels":[],"label_agreement":null},{"id":"W1497590817","doi":"10.1002/2014jb011108","title":"A brittle failure model for long‐period seismic events recorded at Turrialba Volcano, Costa Rica","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Science Foundation Ireland","keywords":"Seismology; Volcano; Geology; Impact crater; Brittleness; Isotropy; Shear (geology); Moment tensor; Waveform; Scaling; Dipole; Magnitude (astronomy); Inversion (geology); Scaling law; Modal; Physics; Tectonics; Mathematics; Radar; Geometry; Materials science; Engineering; Astrophysics; Petrology; Optics","score_opus":0.08055019344567912,"score_gpt":0.33641923505220295,"score_spread":0.2558690416065238,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1497590817","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97735345,0.00021005957,0.018981064,0.00021798458,0.000009854053,0.000031909174,0.000414159,0.00013328422,0.0026481263],"genre_scores_gemma":[0.9987453,0.000054337044,0.0006118411,0.000006683917,0.000003888027,0.000010969116,0.00010648613,0.000011014643,0.0004494724],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991906,0.000024685372,0.0000054452416,0.000018403103,0.000013054024,0.000019312129],"domain_scores_gemma":[0.9998087,0.00006409425,0.000050806408,0.000020622103,0.00003529768,0.000020476338],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035703616,0.00061887264,0.00032121016,0.00064610783,0.00032264407,0.0005079875,0.00095268677,0.00056690624,0.0010245558],"category_scores_gemma":[0.0008716136,0.00031849806,0.0004931199,0.00032107852,0.00037158537,0.0003129131,0.00036088921,0.00030962654,0.00016000649],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006465807,0.000043516975,0.033592723,0.00002947096,0.000058656642,0.00033755534,0.00011600555,0.95523465,0.0037454104,0.0021532958,0.0003778557,0.004246272],"study_design_scores_gemma":[0.0000030087438,0.000006992978,0.0052593993,0.0000021369133,0.0000049566265,0.00001505157,0.000015181531,0.994383,0.000058544116,0.00016986213,0.00007858042,0.000003287046],"about_ca_topic_score_codex":0.06424277,"about_ca_topic_score_gemma":0.037004624,"teacher_disagreement_score":0.06424277,"about_ca_system_score_codex":0.00086844095,"about_ca_system_score_gemma":0.000660647,"threshold_uncertainty_score":0.1277377},"labels":[],"label_agreement":null},{"id":"W1499131702","doi":"10.1002/2013jb010221","title":"Magnetotelluric investigations of the lithosphere beneath the central Rae craton, mainland Nunavut, Canada","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"University of Alberta","keywords":"Craton; Geology; Magnetotellurics; Lithosphere; Crust; Mantle (geology); Archean; Geochemistry; Tectonics; Petrology; Seismology; Electrical resistivity and conductivity","score_opus":0.021612018720385165,"score_gpt":0.2698005003772951,"score_spread":0.24818848165690993,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1499131702","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.994799,0.0004104796,0.00015902115,0.00007702187,0.000003860724,0.000017552997,0.001279757,0.000027966673,0.003225265],"genre_scores_gemma":[0.9972389,0.00017543594,0.00037212807,0.000025711055,0.0000021622225,0.000008689277,0.0005658766,0.000004944376,0.0016061772],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998872,0.0000051887773,0.000004232865,0.00002854247,0.00003966011,0.000035003864],"domain_scores_gemma":[0.99968004,0.00002034858,0.000026640198,0.000012208257,0.00021094711,0.00004978264],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001321827,0.00028163934,0.00016105286,0.0011858868,0.001301569,0.0005945454,0.00046919423,0.00019521292,0.0010908144],"category_scores_gemma":[0.0003592832,0.00019601213,0.00013051467,0.0012619621,0.00054057216,0.00015540679,0.00046349916,0.00020687644,0.00015353794],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014298834,0.000033411012,0.93700755,0.00008587465,0.00008579083,0.00053814915,0.0036851615,0.0028212736,0.02091503,0.00046180972,0.0016079593,0.032614972],"study_design_scores_gemma":[0.000006449787,0.000011570102,0.99533635,0.000022348328,0.000009320275,0.000059215454,0.0011661549,0.00079435343,0.0005895912,0.00003158365,0.0019635628,0.000009544739],"about_ca_topic_score_codex":0.9807402,"about_ca_topic_score_gemma":0.99404955,"teacher_disagreement_score":0.01925981,"about_ca_system_score_codex":0.006296832,"about_ca_system_score_gemma":0.0055548223,"threshold_uncertainty_score":0.0456869},"labels":[],"label_agreement":null},{"id":"W1502075163","doi":"10.1002/jgrb.50114","title":"Low shear velocities in the sub‐lithospheric mantle beneath the Indian shield?","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Ministry of Education, India; Ministry of Earth Sciences","keywords":"Geology; Indian Shield; Lithosphere; Craton; Discontinuity (linguistics); Shield; Seismology; Classification of discontinuities; Mantle (geology); Mantle plume; Archean; Precambrian; Shear zone; Transition zone; Plume; Crust; Shear (geology); Baltic Shield; Geophysics; Petrology; Geochemistry; Tectonics","score_opus":0.024072411896120326,"score_gpt":0.27876451179820955,"score_spread":0.25469209990208924,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1502075163","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99934334,0.000040129395,0.00010825723,0.0000051726784,5.6546946e-7,5.775271e-7,0.00008768551,0.0000107518945,0.00040353014],"genre_scores_gemma":[0.99977106,0.000019106054,0.000056075536,0.0000010478208,6.9826535e-7,3.6186756e-7,0.00007323295,0.0000010288985,0.00007731299],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999716,0.0000019793054,0.0000015452789,0.0000065706085,0.000005379509,0.0000129275595],"domain_scores_gemma":[0.9998965,0.000018868475,0.000037046513,0.000007783602,0.000022168326,0.000017582759],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000055420816,0.00014634336,0.00009642453,0.0007355907,0.0001313374,0.00042745576,0.00016797596,0.00012556156,0.0011716422],"category_scores_gemma":[0.00021982107,0.00011892907,0.00008972673,0.00071828545,0.00014495302,0.00015099614,0.00022926393,0.00012078685,0.00022355275],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030823206,0.000018821256,0.8678794,0.000038332582,0.000043767246,0.00030220603,0.0008400522,0.0007846761,0.113946564,0.0002349042,0.000106468215,0.015496517],"study_design_scores_gemma":[0.0000019638928,0.000029005267,0.9954331,0.0000033867202,0.000014611076,0.000108232256,0.0003938587,0.00062285236,0.0031168736,0.000037399965,0.00023470697,0.0000040220866],"about_ca_topic_score_codex":0.010866347,"about_ca_topic_score_gemma":0.007847861,"teacher_disagreement_score":0.010866347,"about_ca_system_score_codex":0.00014155179,"about_ca_system_score_gemma":0.00013098457,"threshold_uncertainty_score":0.021606207},"labels":[],"label_agreement":null},{"id":"W1512043619","doi":"10.1002/jgrb.50138","title":"Influence of offset weak zones on the development of rift basins: Activation and abandonment during continental extension and breakup","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Dalhousie University","keywords":"Rift; Geology; Lithosphere; Breakup; Necking; Seismology; Offset (computer science); Crust; Petrology; Geophysics; Tectonics; Mechanics; Physics","score_opus":0.022020508663206605,"score_gpt":0.2570000828473654,"score_spread":0.23497957418415882,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1512043619","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973537,0.000111653346,0.001044893,0.000051348907,0.0000039964316,0.000008769963,0.00014471328,0.00002517677,0.001255684],"genre_scores_gemma":[0.9991749,0.000058943213,0.0005008138,0.0000068832746,0.0000013460619,0.000009535642,0.00008042196,0.000008057977,0.0001591646],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998419,0.000049082293,0.000015669431,0.000036560115,0.000017825201,0.000038940096],"domain_scores_gemma":[0.9990637,0.00047170615,0.00022079262,0.00006968437,0.000059019054,0.00011502199],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045073216,0.00051804294,0.00053434103,0.0005066695,0.00043260178,0.0011730616,0.0006188859,0.0009841102,0.0011362431],"category_scores_gemma":[0.0024129797,0.0004469191,0.00084404426,0.00040070276,0.00077869237,0.00062021473,0.0008293146,0.0006092428,0.000115473194],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015744889,0.000066218105,0.05322278,0.000053350264,0.00009075463,0.00019355578,0.00012038386,0.9325018,0.010260762,0.0009764051,0.00007863422,0.00227801],"study_design_scores_gemma":[0.000030102048,0.000087012326,0.020965628,0.000011965422,0.000034382796,0.000037944636,0.00008051516,0.9764904,0.001749377,0.0003163113,0.00017838216,0.00001796358],"about_ca_topic_score_codex":0.015604296,"about_ca_topic_score_gemma":0.009783668,"teacher_disagreement_score":0.015604296,"about_ca_system_score_codex":0.0008235329,"about_ca_system_score_gemma":0.00053300906,"threshold_uncertainty_score":0.0310269},"labels":[],"label_agreement":null},{"id":"W1512502938","doi":"10.1002/2015jb011892","title":"High‐resolution imaging of rapid tremor migrations beneath southern Vancouver Island using cross‐station cross correlations","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Front (military); Seismology; Wavefront; Geodesy; Shear (geology); Physics; Optics","score_opus":0.06330754210976347,"score_gpt":0.34433453206376774,"score_spread":0.28102698995400427,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1512502938","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98815876,0.0002658856,0.004769795,0.00008793525,0.000017164873,0.00003123347,0.0012268962,0.00022822335,0.0052141175],"genre_scores_gemma":[0.9912135,0.00016190104,0.006239003,0.000037320035,0.000018748198,0.000017982296,0.00094394357,0.000041990468,0.0013255865],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985576,0.000010146633,0.000004493867,0.000032190503,0.00005627219,0.00004107459],"domain_scores_gemma":[0.9995485,0.00003923698,0.00004201396,0.000029523046,0.0002760518,0.00006462475],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021861089,0.0003170324,0.00017915656,0.0020507944,0.00041209316,0.0006436721,0.0003334129,0.00028243876,0.0015715342],"category_scores_gemma":[0.0005817218,0.00026895065,0.00015080262,0.0015325784,0.00013716459,0.00021523202,0.00049433456,0.00029699306,0.00035100617],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026274574,0.0002587887,0.50632703,0.00017462224,0.00040055803,0.0008882828,0.0011217461,0.012024057,0.34203428,0.0005407036,0.005714599,0.13025257],"study_design_scores_gemma":[0.000012959714,0.000031721294,0.9570895,0.000022741666,0.00005583579,0.00016183793,0.00032390916,0.032297906,0.007601695,0.000085678126,0.0022899737,0.00002623998],"about_ca_topic_score_codex":0.12341447,"about_ca_topic_score_gemma":0.32842195,"teacher_disagreement_score":0.87658554,"about_ca_system_score_codex":0.00051761523,"about_ca_system_score_gemma":0.0009230442,"threshold_uncertainty_score":0.2453922},"labels":[],"label_agreement":null},{"id":"W1514598599","doi":"10.1002/jgrb.50243","title":"The shallow structure of Kīlauea caldera from high‐resolution Bouguer gravity and total magnetic anomaly mapping: Insights into progressive magma reservoir growth","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Caldera; Bouguer anomaly; Geology; Volcano; Impact crater; Gravity anomaly; Seismology; Magnetic anomaly; Magma; Rift; Rift zone; Magma chamber; Free-air gravity anomaly; Geophysics; Petrology; Geomorphology; Paleontology; Tectonics","score_opus":0.010090402123007665,"score_gpt":0.261497827891279,"score_spread":0.25140742576827135,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1514598599","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987312,0.00009397056,0.00038000193,0.000031638323,0.0000015995879,0.000004194373,0.00018701097,0.000057472203,0.00051302667],"genre_scores_gemma":[0.9992066,0.000022732833,0.00053675356,0.000005830028,0.0000014851571,0.0000024527308,0.00010866482,0.000004576299,0.00011103241],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999621,0.0000041517565,0.0000014901561,0.000011502571,0.000009112926,0.000011610668],"domain_scores_gemma":[0.99990535,0.000013667753,0.00001678684,0.000008967182,0.000030063253,0.000025174353],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012413962,0.00021581234,0.00017199792,0.0008627212,0.0002498528,0.00047600808,0.00023959432,0.0002071828,0.0007286682],"category_scores_gemma":[0.00029865297,0.00015102292,0.00012632452,0.0004706288,0.0001968193,0.0002472284,0.00023455657,0.00016955636,0.00008630784],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015633683,0.000047652586,0.87890446,0.00005477127,0.00008925143,0.0005725975,0.0018517426,0.00906228,0.081769966,0.00030500986,0.0006611705,0.02652481],"study_design_scores_gemma":[0.000006501163,0.000014142988,0.9832239,0.0000070192514,0.000014066383,0.000047665948,0.00032227105,0.014427307,0.0013635955,0.00004359165,0.0005225964,0.0000072485955],"about_ca_topic_score_codex":0.09825508,"about_ca_topic_score_gemma":0.19385888,"teacher_disagreement_score":0.09825508,"about_ca_system_score_codex":0.00060551247,"about_ca_system_score_gemma":0.0002771079,"threshold_uncertainty_score":0.19536638},"labels":[],"label_agreement":null},{"id":"W1525966310","doi":"10.1029/2012jb009651","title":"Tidal calibration of plate boundary observatory borehole strainmeters","year":2012,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":69,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Borehole; Coupling (piping); Geology; Geodesy; Observatory; Boundary (topology); GNSS applications; Geodetic datum; Seismology; Geophysics; Physics; Geotechnical engineering; Mathematics; Mathematical analysis; Satellite; Astrophysics; Materials science","score_opus":0.06010335255071511,"score_gpt":0.31778430457919116,"score_spread":0.2576809520284761,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1525966310","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9566819,0.000064424574,0.03665695,0.00007318049,0.000046347952,0.00011998378,0.0015204751,0.00039139218,0.0044453577],"genre_scores_gemma":[0.9592187,0.00004810061,0.037465528,0.00004791034,0.000011347376,0.00010325339,0.002367666,0.00009675155,0.00064083585],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980287,0.00034711784,0.0001443291,0.0003513558,0.000984831,0.000143585],"domain_scores_gemma":[0.99557424,0.0007713667,0.0007224168,0.0011387375,0.0016246,0.00016860367],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002465601,0.00042757558,0.0002623041,0.0008816401,0.00053724716,0.00067579263,0.0009030122,0.00045633267,0.0010061029],"category_scores_gemma":[0.010465584,0.00039586678,0.00019473162,0.0016267573,0.0004009991,0.0007210256,0.00083311205,0.00043095334,0.00042152285],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025928335,0.00022220486,0.8323804,0.000056142017,0.000088407636,0.00005629186,0.00066650554,0.02017057,0.04130049,0.0011032338,0.0020017864,0.10169471],"study_design_scores_gemma":[0.00008999435,0.00026101273,0.9218293,0.00002852955,0.00004178167,0.00010033059,0.00027334833,0.046696175,0.025131973,0.0005026164,0.0049911947,0.00005376725],"about_ca_topic_score_codex":0.012977464,"about_ca_topic_score_gemma":0.030078286,"teacher_disagreement_score":0.012977464,"about_ca_system_score_codex":0.0007394634,"about_ca_system_score_gemma":0.0011248845,"threshold_uncertainty_score":0.025803804},"labels":[],"label_agreement":null},{"id":"W1531280820","doi":"10.1002/2015jb011963","title":"Frictional properties of the active San Andreas Fault at SAFOD: Implications for fault strength and slip behavior","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":121,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"National Science Foundation","keywords":"Geology; Borehole; Slip (aerodynamics); Seismology; Fault (geology); Creep; San andreas fault; Geotechnical engineering; Petrology; Materials science; Composite material","score_opus":0.10594517933876572,"score_gpt":0.3421397163003114,"score_spread":0.2361945369615457,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1531280820","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992594,0.000039158916,0.00016086941,0.000009055159,8.5408504e-7,0.0000030870096,0.00014155296,0.000013464191,0.00037247138],"genre_scores_gemma":[0.99955815,0.000023500099,0.00015250932,0.000004824356,0.0000013000862,0.000002748256,0.00012755483,0.0000027389833,0.00012663922],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984896,0.0000093665585,0.000010348128,0.000046600762,0.000056191584,0.000028528886],"domain_scores_gemma":[0.99975413,0.0000281373,0.000075559576,0.00003369052,0.000069482856,0.0000389858],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021414855,0.00031640643,0.0004517867,0.0008035589,0.00046738394,0.000478344,0.0003606698,0.00031839847,0.0006287196],"category_scores_gemma":[0.00047313914,0.0002155115,0.00020841161,0.0005529222,0.000440769,0.00030465279,0.00030658106,0.0002566526,0.00017369578],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018047454,0.00010505424,0.79972994,0.00006576428,0.00009282993,0.0002636061,0.0004954082,0.003207008,0.18916823,0.00017532961,0.00011457479,0.0064018327],"study_design_scores_gemma":[0.0000063418865,0.00006573819,0.9857384,0.0000053055596,0.000014857773,0.00008842625,0.00018422531,0.0032831097,0.010218062,0.00003704999,0.00035041766,0.000008050161],"about_ca_topic_score_codex":0.02251592,"about_ca_topic_score_gemma":0.03159618,"teacher_disagreement_score":0.02251592,"about_ca_system_score_codex":0.0006175104,"about_ca_system_score_gemma":0.00031074614,"threshold_uncertainty_score":0.044769704},"labels":[],"label_agreement":null},{"id":"W1531499868","doi":"10.1002/2014jb010998","title":"Rapid erosion of the Southern African Plateau as it climbs over a mantle superswell","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":123,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Agence Nationale de la Recherche; Canadian Institute for Advanced Research","keywords":"Geology; Denudation; Sedimentary rock; Mantle (geology); Plateau (mathematics); Volcanic plateau; Paleontology; Fluvial; Quaternary; Geomorphology; Volcano; Tectonics; Volcanic rock; Structural basin","score_opus":0.03006154474819775,"score_gpt":0.27658969133380734,"score_spread":0.2465281465856096,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1531499868","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992435,0.000080559366,0.00008660902,0.000021721893,0.0000011910149,8.65835e-7,0.00007072052,0.000009038804,0.00048579994],"genre_scores_gemma":[0.9996985,0.000057977904,0.000082058476,0.0000034859138,0.0000020791376,7.2511165e-7,0.000075313226,0.0000013008479,0.000078481964],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996746,0.000005094026,0.0000020880775,0.0000087654,0.000008550477,0.000007915142],"domain_scores_gemma":[0.99986756,0.000021286416,0.00004717826,0.000017060096,0.000026875876,0.000020028114],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011940964,0.000114256974,0.00012375067,0.0006030397,0.00022116321,0.00038811567,0.000094082265,0.00013369229,0.0011940206],"category_scores_gemma":[0.0003142405,0.00007032767,0.00009644383,0.0006370228,0.0001719484,0.00024234879,0.00021529871,0.00016140538,0.000108298984],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024333903,0.00004226135,0.8125544,0.000075041775,0.00009807652,0.001324909,0.00065455626,0.0040033446,0.15421075,0.00074684905,0.00045466484,0.025591774],"study_design_scores_gemma":[0.0000043363825,0.000038919472,0.99412054,0.000004802163,0.000009564041,0.0001494187,0.00013395493,0.0026918603,0.001982186,0.00012115214,0.0007395126,0.0000038057062],"about_ca_topic_score_codex":0.0039091716,"about_ca_topic_score_gemma":0.005278757,"teacher_disagreement_score":0.0039091716,"about_ca_system_score_codex":0.00023435382,"about_ca_system_score_gemma":0.00010355122,"threshold_uncertainty_score":0.007772863},"labels":[],"label_agreement":null},{"id":"W1534014660","doi":"10.1002/jgrb.50220","title":"Influence of viscosity pressure dependence on deep lithospheric tectonics during continental collision","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Lithosphere; Geology; Subduction; Mantle (geology); Continental collision; Collision zone; Mantle convection; Geophysics; Tectonics; Petrology; Seismology","score_opus":0.01304457261042342,"score_gpt":0.27589102561061735,"score_spread":0.26284645300019394,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1534014660","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99800545,0.000120262266,0.00059348514,0.000044352953,0.0000064332385,0.000005736505,0.00013526596,0.00003752051,0.0010515774],"genre_scores_gemma":[0.99982244,0.000030828767,0.000052433094,0.0000030569997,0.0000012964772,0.000002417848,0.00003819274,0.0000047910794,0.00004453089],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99984336,0.00004083057,0.000012589475,0.000037003407,0.000025158153,0.000040969826],"domain_scores_gemma":[0.9989365,0.0007080527,0.00011304996,0.00010240013,0.00005193169,0.00008816137],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032922174,0.0003508543,0.0003531412,0.00039682043,0.00031920755,0.000945561,0.00033119338,0.00048664835,0.0014117642],"category_scores_gemma":[0.0022446027,0.00024676824,0.00029516616,0.00032117864,0.0007681458,0.0004871705,0.0006634596,0.00061131176,0.00013850017],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016866538,0.00039830396,0.07793365,0.0002027811,0.00017732236,0.00086630357,0.00034236402,0.48832983,0.41292587,0.0023074215,0.00037844814,0.014451077],"study_design_scores_gemma":[0.00019325636,0.0013706534,0.19243856,0.000034045603,0.0001347853,0.00022270989,0.00023059508,0.6691143,0.13388312,0.0011193132,0.0011356281,0.00012298702],"about_ca_topic_score_codex":0.0028103509,"about_ca_topic_score_gemma":0.00080813176,"teacher_disagreement_score":0.0028103509,"about_ca_system_score_codex":0.00053492736,"about_ca_system_score_gemma":0.00022118451,"threshold_uncertainty_score":0.005587995},"labels":[],"label_agreement":null},{"id":"W1535559137","doi":"10.1002/2014jb011643","title":"Ice sheet load cycling and fluid underpressures in the Eastern Michigan Basin, Ontario, Canada","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey; Nuclear Waste Management Organization","keywords":"Geology; Glacial period; Aquifer; Ice sheet; Last Glacial Maximum; Structural basin; Geomorphology; Groundwater; Geotechnical engineering","score_opus":0.03317484789112824,"score_gpt":0.2781324885739895,"score_spread":0.24495764068286124,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1535559137","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99629056,0.000091644986,0.000095957424,0.00010046177,0.0000020941486,0.000011065744,0.0011090726,0.000014066402,0.0022850684],"genre_scores_gemma":[0.9983523,0.00009494516,0.0001776616,0.00001290084,8.8620567e-7,0.00000572283,0.00038731878,0.0000042270003,0.0009641628],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987924,0.000010425628,0.000006264077,0.000029229135,0.000039331015,0.000035425823],"domain_scores_gemma":[0.9994879,0.000063881,0.00006763285,0.000020575928,0.00026519434,0.00009469261],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018732851,0.00022071009,0.00017071854,0.0005606306,0.001672759,0.00090734265,0.00057341764,0.00028143724,0.0018946878],"category_scores_gemma":[0.0008223327,0.0002113944,0.00021326136,0.0011083959,0.0006185286,0.00032834723,0.00035384655,0.00018158977,0.00013704196],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001293391,0.000033977674,0.9749203,0.00004944661,0.000099249184,0.00023575354,0.001284462,0.0101867635,0.0028456745,0.0004936978,0.0017833608,0.007937977],"study_design_scores_gemma":[0.000011809107,0.000012048856,0.9843051,0.000015016323,0.000029332617,0.000031565156,0.0012380797,0.011334305,0.00048268007,0.000095741336,0.0024270148,0.000017444625],"about_ca_topic_score_codex":0.9956104,"about_ca_topic_score_gemma":0.9984376,"teacher_disagreement_score":0.026115514,"about_ca_system_score_codex":0.026115514,"about_ca_system_score_gemma":0.013338226,"threshold_uncertainty_score":0.18948221},"labels":[],"label_agreement":null},{"id":"W1556293097","doi":"10.1002/jgrb.50060","title":"Modification of continental lithosphere by tectonic processes: A tomographic image of central North America","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal; University of Manitoba","funders":"Natural Sciences and Engineering Research Council of Canada; Manitoba Hydro","keywords":"Geology; Terrane; Rift; Lithosphere; Proterozoic; Gondwana; Seismology; Orogeny; Laurentia; Precambrian; Tectonics; Paleontology","score_opus":0.015545024852970882,"score_gpt":0.27522410765621813,"score_spread":0.25967908280324725,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1556293097","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949856,0.00023009983,0.00010716373,0.00006698707,0.00000406419,0.000013571121,0.0012682918,0.00006194724,0.0032624349],"genre_scores_gemma":[0.9976866,0.00023349939,0.0007406826,0.000020459085,0.0000076174115,0.000008657999,0.0006617198,0.000009088939,0.00063163304],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999972,0.000001254498,0.0000013883907,0.000009050872,0.000008139375,0.000008169261],"domain_scores_gemma":[0.99988556,0.000008818198,0.00002401451,0.0000073991237,0.00004069895,0.000033576904],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000053174022,0.0002400235,0.00011934828,0.0010991896,0.0004846423,0.0006479803,0.00024732907,0.00022759149,0.0014850101],"category_scores_gemma":[0.00013413219,0.00018453965,0.00013745422,0.0015998161,0.0002344365,0.00021622612,0.00029428524,0.00014811389,0.0001511402],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036996513,0.00023833157,0.85527664,0.00020708323,0.00023037102,0.0017762339,0.0038934513,0.009609165,0.057400867,0.00082966516,0.0074398867,0.06272835],"study_design_scores_gemma":[0.000014495313,0.0000118876405,0.99188715,0.000022471215,0.000040282506,0.00012130783,0.0006491406,0.0044917497,0.00039947018,0.000051167444,0.002303149,0.000007727324],"about_ca_topic_score_codex":0.3650416,"about_ca_topic_score_gemma":0.612231,"teacher_disagreement_score":0.3650416,"about_ca_system_score_codex":0.0013660074,"about_ca_system_score_gemma":0.001194156,"threshold_uncertainty_score":0.72583365},"labels":[],"label_agreement":null},{"id":"W1559584481","doi":"10.1002/2014jb011802","title":"Sharp mantle transition from cratons to Cordillera in southwestern Canada","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Helmholtz-Alberta Initiative","keywords":"Geology; Craton; Mantle (geology); Lithosphere; Transition zone; Foreland basin; Subduction; Terrane; Seismology; Crust; Paleontology; Geophysics; Tectonics","score_opus":0.048504575349437896,"score_gpt":0.3013517490641233,"score_spread":0.2528471737146854,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1559584481","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966067,0.0002405589,0.000035375335,0.00008812368,0.0000029114792,0.000005815003,0.00073291565,0.000010462883,0.0022770036],"genre_scores_gemma":[0.9985461,0.00012591062,0.00006825446,0.000018393826,0.0000011552434,0.0000021066303,0.00044781182,0.0000029062264,0.00078741217],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998833,0.00000334461,0.0000033712536,0.000028231307,0.000024757483,0.000056955214],"domain_scores_gemma":[0.99980074,0.000009952708,0.00003253836,0.0000057171196,0.00010368042,0.000047330035],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007773274,0.00019079988,0.00017442205,0.0014910231,0.0011537963,0.00091116194,0.00041547438,0.00020840207,0.0024683764],"category_scores_gemma":[0.00037064374,0.000114785515,0.00013238515,0.0024490594,0.00045403972,0.00018203081,0.0005977591,0.0002038452,0.00015335256],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013996707,0.000018025692,0.966142,0.00004623056,0.000046297188,0.00051138253,0.0020551945,0.0005998622,0.0070836283,0.00043472007,0.0012160464,0.021706833],"study_design_scores_gemma":[0.0000018666548,0.000002704037,0.997843,0.000008939161,0.0000056248823,0.00002878766,0.0010307078,0.00015742377,0.00012367427,0.000017437467,0.0007770659,0.0000026301816],"about_ca_topic_score_codex":0.98072076,"about_ca_topic_score_gemma":0.9933102,"teacher_disagreement_score":0.019279242,"about_ca_system_score_codex":0.007922407,"about_ca_system_score_gemma":0.005892638,"threshold_uncertainty_score":0.057481408},"labels":[],"label_agreement":null},{"id":"W1560878246","doi":"10.1002/2014jb011644","title":"Resonant seismic and microseismic ground motion of the Cascadia subduction zone accretionary prism and implications for seismic velocity","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Ocean Networks Canada Society; University of Victoria; Geological Survey of Canada","funders":"National Science Foundation","keywords":"Geology; Seismology; Accretionary wedge; Microseism; Subduction; Seafloor spreading; Swell; Prism; Geophysics; Tectonics; Oceanography","score_opus":0.0281980402603601,"score_gpt":0.2953766772641539,"score_spread":0.2671786370037938,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1560878246","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985719,0.000014137307,0.000087177075,0.000028389595,0.0000022073611,0.0000021742896,0.0001989305,0.000011590679,0.0010834933],"genre_scores_gemma":[0.9997253,0.0000070705546,0.000046226265,0.0000035083192,7.512564e-7,0.0000011225587,0.00008574768,0.0000017226271,0.00012860177],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986184,0.000013077935,0.000008620328,0.00004633675,0.000030422889,0.000039738155],"domain_scores_gemma":[0.99963415,0.000043901902,0.00006590437,0.000033596614,0.00011730118,0.00010519012],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001733905,0.00022413454,0.00015072843,0.0007311215,0.0003985066,0.00031614501,0.00032546313,0.00024574477,0.0016537335],"category_scores_gemma":[0.0010194058,0.00018689122,0.00017632365,0.000610801,0.00035739015,0.00015863501,0.00041954074,0.00019196357,0.00022339805],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015998872,0.000030686853,0.9621069,0.000025571695,0.000034483044,0.00030354242,0.00053030776,0.001582974,0.030565184,0.000092535134,0.0001917899,0.0043761185],"study_design_scores_gemma":[0.0000012109197,0.0000066793823,0.99914765,0.000001234359,0.0000020607474,0.000022395427,0.00014143213,0.00040709367,0.00019109888,0.0000084949725,0.00006912397,0.0000015610904],"about_ca_topic_score_codex":0.14068288,"about_ca_topic_score_gemma":0.17814466,"teacher_disagreement_score":0.14068288,"about_ca_system_score_codex":0.0011900669,"about_ca_system_score_gemma":0.0005552412,"threshold_uncertainty_score":0.279728},"labels":[],"label_agreement":null},{"id":"W1560880907","doi":"10.1002/2014jb011463","title":"Paleomagnetism of the ~1.1 Ga Coldwell Complex (Ontario, Canada): Implications for Proterozoic geomagnetic field morphology and plate velocities","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Paleomagnetism; Geology; Geomagnetic pole; Earth's magnetic field; Paleontology; Polarity (international relations); Geomagnetic reversal; Laurentia; Proterozoic; Rift; Volcanic rock; Polar wander; Geophysics; Asymmetry; Seismology; Volcano; Paleozoic; Magnetic field; Tectonics; Physics","score_opus":0.025999205183319638,"score_gpt":0.29119357320311107,"score_spread":0.2651943680197914,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1560880907","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9918154,0.00030855802,0.000120751734,0.00010619962,0.000004097405,0.000012803079,0.0014055968,0.000016251657,0.0062101735],"genre_scores_gemma":[0.99823284,0.00009605321,0.00011992028,0.000019900232,0.0000015697499,0.000004112755,0.0003909987,0.000005869446,0.0011288611],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998776,0.0000030441058,0.0000043675054,0.00003515957,0.000042475378,0.000037362435],"domain_scores_gemma":[0.9995722,0.000018546294,0.00007657146,0.000017178168,0.0002534447,0.00006204354],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001096716,0.0002366506,0.00023287171,0.0017892886,0.0019640275,0.0009722002,0.0006387551,0.00025042612,0.0024011815],"category_scores_gemma":[0.0004458442,0.00018904929,0.00018014116,0.0017186833,0.00097579753,0.00021323269,0.00044372768,0.0002577109,0.00025724695],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016313556,0.000018632807,0.95728576,0.000064677995,0.000069819966,0.0003027937,0.0024430659,0.00086001045,0.024956943,0.0006075093,0.00096270046,0.012264987],"study_design_scores_gemma":[0.0000028307354,0.0000037845953,0.9977385,0.000006856665,0.0000062820163,0.000033579334,0.00037332837,0.00016044329,0.00034271623,0.000020673922,0.0013069793,0.000004018236],"about_ca_topic_score_codex":0.98402804,"about_ca_topic_score_gemma":0.9934157,"teacher_disagreement_score":0.016391328,"about_ca_system_score_codex":0.016391328,"about_ca_system_score_gemma":0.006049402,"threshold_uncertainty_score":0.118927956},"labels":[],"label_agreement":null},{"id":"W1562504550","doi":"10.1002/2014jb011176","title":"Space geodesy constrains ice age terminal deglaciation: The global ICE‐6G_C (VM5a) model","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":1510,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; National Oceanic and Atmospheric Administration","keywords":"Deglaciation; Post-glacial rebound; Geology; Geodetic datum; Geodesy; Global Positioning System; Gravitational field; Ice sheet; Climatology; Glacial period; Oceanography; Paleontology; Computer science","score_opus":0.04792835078421767,"score_gpt":0.3423926485958936,"score_spread":0.29446429781167593,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1562504550","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.84979874,0.00096520735,0.08461058,0.0017936606,0.00029554774,0.000093413415,0.0076985746,0.00077557855,0.053968713],"genre_scores_gemma":[0.99218726,0.00016732136,0.004327246,0.00006258768,0.0000412606,0.000032902535,0.0012443472,0.000058714762,0.0018783646],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998951,0.000033417466,0.000004843693,0.00002690852,0.000016627275,0.000023104067],"domain_scores_gemma":[0.99976,0.000086198816,0.00003492772,0.000023674922,0.000055818702,0.000039473765],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004236458,0.0005336939,0.0004502355,0.00055796833,0.00045080562,0.0012710879,0.0012350067,0.0008459303,0.0025136624],"category_scores_gemma":[0.00094616483,0.000248822,0.000626575,0.000644245,0.00046960343,0.0005874643,0.0005478556,0.0004788362,0.0005336969],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000022966236,0.000006214734,0.00436534,0.000007854407,0.00001550459,0.000022665792,0.000010957514,0.9908949,0.00015273251,0.0023883432,0.0005941018,0.0015184506],"study_design_scores_gemma":[0.000024644882,0.0000137717325,0.0025599182,0.000008336234,0.000013657186,0.0000105839945,0.000012574296,0.9936551,0.000105000225,0.0018139195,0.0017754056,0.00000718057],"about_ca_topic_score_codex":0.08951717,"about_ca_topic_score_gemma":0.043258995,"teacher_disagreement_score":0.08951717,"about_ca_system_score_codex":0.0012928784,"about_ca_system_score_gemma":0.0013434842,"threshold_uncertainty_score":0.17799228},"labels":[],"label_agreement":null},{"id":"W1570914366","doi":"10.1002/2013jb010578","title":"The long‐wavelength admittance and effective elastic thickness of the Canadian Shield","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Craton; Lithosphere; Indian Shield; Crust; Mantle (geology); Shield; Seismology; Convection; Geophysics; Wavelength; Admittance; Geodesy; Tectonics; Petrology; Mechanics; Physics","score_opus":0.019611468512191116,"score_gpt":0.2834648703866294,"score_spread":0.2638534018744383,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1570914366","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99556255,0.00008222641,0.0006496549,0.00003709198,0.0000022993024,0.000004665811,0.00096698914,0.000017679205,0.0026768777],"genre_scores_gemma":[0.99905306,0.000041501724,0.00024770483,0.0000050247722,8.28895e-7,0.0000012638355,0.0002586366,0.0000034495783,0.0003884838],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987805,0.0000042726697,0.000004074429,0.000021802953,0.000058816906,0.000033003616],"domain_scores_gemma":[0.99958175,0.000041597687,0.000058598398,0.000013344936,0.000255109,0.000049566755],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014870599,0.00035183554,0.000114436,0.001598521,0.0008713096,0.0007117694,0.00043687256,0.00020930155,0.0020409205],"category_scores_gemma":[0.0006801102,0.00012465587,0.00017233871,0.0015529527,0.00049678003,0.00026411592,0.00032870614,0.00017413772,0.00017693569],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018867034,0.000028405617,0.91040784,0.00007350227,0.00014614548,0.0005341977,0.0009429022,0.013611213,0.035877567,0.0018369908,0.0010248242,0.035327747],"study_design_scores_gemma":[0.0000023994044,0.000004053606,0.99294734,0.0000066929238,0.000008783924,0.00005350646,0.00037983325,0.004470965,0.0013981148,0.0001193956,0.0005962881,0.000012499295],"about_ca_topic_score_codex":0.92639107,"about_ca_topic_score_gemma":0.95131856,"teacher_disagreement_score":0.073608935,"about_ca_system_score_codex":0.0047250288,"about_ca_system_score_gemma":0.0025766396,"threshold_uncertainty_score":0.14808482},"labels":[],"label_agreement":null},{"id":"W1580211932","doi":"10.1002/jgrb.50201","title":"Factors controlling early stage salt tectonics at rifted continental margins and their thermal consequences","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Newfoundland and Labrador Centre for Applied Health Research; ExxonMobil (Canada); Dalhousie University","funders":"","keywords":"Geology; Salt tectonics; Diapir; Aggradation; Geomorphology; Petrology; Halite; Salt dome; Continental margin; Subsidence; Tectonics; Structural basin; Paleontology","score_opus":0.03299614693225328,"score_gpt":0.2829118256949317,"score_spread":0.2499156787626784,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1580211932","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989416,0.000021603993,0.00046575817,0.000024490526,0.0000012169022,0.0000026226219,0.00006685917,0.000011552144,0.0004642626],"genre_scores_gemma":[0.99982303,0.000008574636,0.00007223271,0.0000024026306,5.577172e-7,0.0000013076598,0.000024662933,0.0000033510107,0.00006385077],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99991345,0.000021177722,0.000006622875,0.000028612854,0.000010153385,0.00001991608],"domain_scores_gemma":[0.9997061,0.00010315462,0.000070183574,0.000026572914,0.000048040023,0.00004591957],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025064326,0.0003015369,0.00028019867,0.00026220482,0.00038722798,0.0009330177,0.0003517475,0.00053433265,0.0018758025],"category_scores_gemma":[0.0014264637,0.0004235315,0.0003329136,0.00021100555,0.0004721862,0.0005265421,0.0004015758,0.00028744596,0.00013738306],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033830505,0.00009006754,0.32682836,0.000090050366,0.00014080088,0.00042517518,0.0002709057,0.5380478,0.12536147,0.003512762,0.00024328129,0.0046510557],"study_design_scores_gemma":[0.00005905586,0.00014304835,0.38980168,0.000011579212,0.000064060536,0.00007590303,0.0001937337,0.596551,0.011445775,0.001215129,0.00038740627,0.000051674757],"about_ca_topic_score_codex":0.011817826,"about_ca_topic_score_gemma":0.010279735,"teacher_disagreement_score":0.011817826,"about_ca_system_score_codex":0.0010185586,"about_ca_system_score_gemma":0.00032318587,"threshold_uncertainty_score":0.023498058},"labels":[],"label_agreement":null},{"id":"W1587056493","doi":"10.1002/2014jb011622","title":"KALREF—A Kalman filter and time series approach to the International Terrestrial Reference Frame realization","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"GNSS positioning and interference","field":"Engineering","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"California Institute of Technology; Jet Propulsion Laboratory; National Aeronautics and Space Administration","keywords":"Reference frame; Kalman filter; Geodesy; Geodetic datum; Series (stratigraphy); Computer science; Frame of reference; Geology; Frame (networking); Artificial intelligence; Telecommunications","score_opus":0.07498805409104675,"score_gpt":0.3239067599920724,"score_spread":0.24891870590102566,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1587056493","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0012201158,0.00006204482,0.9974598,0.00006178937,0.000026233673,0.000011167869,0.000048469443,0.00013818184,0.0009722673],"genre_scores_gemma":[0.28414324,0.0006307356,0.7043653,0.00015043074,0.00025945195,0.000323849,0.0009230392,0.0002137958,0.008990155],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9991861,0.00027376664,0.00005940963,0.0002262316,0.00020186476,0.00005255702],"domain_scores_gemma":[0.99908805,0.0004478848,0.000114761395,0.000080295344,0.0002482887,0.000020617617],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015614205,0.0006612445,0.0007198361,0.0010627847,0.00055316923,0.0014371263,0.0011668274,0.00083416456,0.0044528185],"category_scores_gemma":[0.0038270606,0.00037960056,0.000789416,0.001077769,0.0005834989,0.0016770973,0.00087886775,0.0013128164,0.00088015496],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007257133,0.000042962827,0.00097616256,0.00009043336,0.000059030135,0.000108979264,0.00013773564,0.66236085,0.001294312,0.18231136,0.0025232495,0.15002234],"study_design_scores_gemma":[0.000005186313,0.00001820502,0.00019320048,0.000008890401,0.000006297094,0.0000087917615,0.000011597027,0.9807982,0.00025313415,0.016266989,0.0024181637,0.000011310483],"about_ca_topic_score_codex":0.018029002,"about_ca_topic_score_gemma":0.010758659,"teacher_disagreement_score":0.018029002,"about_ca_system_score_codex":0.0009901121,"about_ca_system_score_gemma":0.0012426629,"threshold_uncertainty_score":0.03584814},"labels":[],"label_agreement":null},{"id":"W1599440120","doi":"10.1002/jgrb.50110","title":"Seismic velocities, anisotropy, and shear‐wave splitting of antigorite serpentinites and tectonic implications for subduction zones","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":91,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Bedford Institute of Oceanography; Polytechnique Montréal","funders":"","keywords":"Geology; Subduction; Seismic anisotropy; Forearc; Mantle (geology); Anisotropy; Shear wave splitting; Shear (geology); Mantle wedge; Tectonics; Peridotite; Mineralogy; Seismology; Geochemistry; Petrology","score_opus":0.041683451132613354,"score_gpt":0.3059987396211144,"score_spread":0.26431528848850105,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1599440120","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997482,0.000035213536,0.000053560696,0.0000026803343,2.8255903e-7,5.401672e-7,0.000035771136,0.000002688711,0.00012113344],"genre_scores_gemma":[0.9997862,0.00002379263,0.00007168135,0.0000012801671,5.6288985e-7,7.938179e-7,0.000068847316,0.0000012879136,0.000045537286],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999167,0.000009784833,0.000009297577,0.00002746146,0.00001912382,0.000017750652],"domain_scores_gemma":[0.9997626,0.000028801449,0.00011694059,0.000017750253,0.000038457547,0.000035389916],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013904735,0.00031789014,0.00013502482,0.0008920294,0.00016638063,0.00036666243,0.000181025,0.00014644091,0.00045524404],"category_scores_gemma":[0.0004105365,0.00018835065,0.000110632485,0.00041849396,0.00042775134,0.00021774259,0.0002759242,0.00015417363,0.00008942444],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045691352,0.00003118976,0.47228068,0.000043335454,0.000034822144,0.00024978342,0.00064242474,0.0010875536,0.51780504,0.00018200999,0.000025511703,0.0071606855],"study_design_scores_gemma":[0.000004660078,0.00004792959,0.9821684,0.0000037382622,0.000009881053,0.00014808222,0.00016405704,0.00089384324,0.01634296,0.00004471591,0.00016605659,0.0000057037037],"about_ca_topic_score_codex":0.003094416,"about_ca_topic_score_gemma":0.0031387364,"teacher_disagreement_score":0.003094416,"about_ca_system_score_codex":0.00020359774,"about_ca_system_score_gemma":0.000089716974,"threshold_uncertainty_score":0.0061528087},"labels":[],"label_agreement":null},{"id":"W1604312882","doi":"10.1002/2014jb011744","title":"Self‐similar rupture implied by scaling properties of volcanic earthquakes occurring during the 2004‐2008 eruption of Mount St. Helens, Washington","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Seismology; Volcano; Scaling; Geology; Impact crater; Seismometer; Geodesy; Physics; Mathematics; Geometry","score_opus":0.0435549921846325,"score_gpt":0.286415734267319,"score_spread":0.2428607420826865,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1604312882","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99958795,0.000007621782,0.00021605226,0.0000044364747,4.626335e-7,0.000001962366,0.000033450462,0.000004710094,0.00014338999],"genre_scores_gemma":[0.9998356,0.000003966879,0.00007481939,0.0000010422912,0.0000011931352,0.0000010783058,0.00006240345,0.0000011001347,0.000018830942],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998665,0.000026506708,0.00001560624,0.000036935722,0.000028706596,0.000025753661],"domain_scores_gemma":[0.9986299,0.00032598706,0.000554331,0.00021270663,0.00014900413,0.00012809581],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033176693,0.00014743555,0.00019286531,0.001434219,0.00025870523,0.0004789081,0.00018295879,0.00021735388,0.00062496145],"category_scores_gemma":[0.0023741608,0.00017902984,0.00027362094,0.000582847,0.00044164743,0.00036145683,0.0002872435,0.00015187437,0.00012519919],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000083358325,0.00006670803,0.980368,0.000008578522,0.0000886783,0.0002329043,0.00020771772,0.008242663,0.0054383655,0.00033514414,0.00014913111,0.0047787516],"study_design_scores_gemma":[0.000002880775,0.000026888687,0.97430336,0.0000020041089,0.000011588749,0.00009641587,0.00011618368,0.024843777,0.00029663107,0.00022843094,0.00006479299,0.0000069835164],"about_ca_topic_score_codex":0.0035848098,"about_ca_topic_score_gemma":0.003823432,"teacher_disagreement_score":0.0035848098,"about_ca_system_score_codex":0.0002791987,"about_ca_system_score_gemma":0.00009916596,"threshold_uncertainty_score":0.007127881},"labels":[],"label_agreement":null},{"id":"W1607824243","doi":"10.1002/jgrb.50155","title":"Particle sedimentation and diffusive convection in volcanic ash‐clouds","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Aeolian processes and effects","field":"Earth and Planetary Sciences","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Settling; Volcanic ash; Sedimentation; Atmospheric sciences; Particle (ecology); Convection; Volcano; Geology; Environmental science; Meteorology; Geomorphology; Geography; Geochemistry; Oceanography","score_opus":0.022859239352280108,"score_gpt":0.3073013426522749,"score_spread":0.28444210329999475,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1607824243","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990778,0.00010348992,0.00051823974,0.000012775673,0.0000033382557,0.000004293168,0.000008480464,0.000007562149,0.00026388947],"genre_scores_gemma":[0.9996518,0.000033409684,0.00020830157,0.0000024926533,0.0000017629701,0.0000019541658,0.000010261218,0.0000012541584,0.000088772744],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99995065,0.000007980008,0.000003911482,0.000011722473,0.000011731789,0.000014057205],"domain_scores_gemma":[0.9998381,0.00005470953,0.00005545948,0.000009880457,0.000011500027,0.000030462812],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015382898,0.00025309942,0.00019278917,0.00026256606,0.00041522947,0.0005217897,0.00022725106,0.00025014835,0.00022644625],"category_scores_gemma":[0.00039714194,0.000187551,0.00017494473,0.00014575398,0.0004011501,0.00026020678,0.00034794817,0.00020119209,0.0000399548],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00072641956,0.00026385946,0.13300447,0.000116599025,0.000086944965,0.0006080085,0.00077056343,0.17084758,0.6762835,0.0050148647,0.00022028702,0.012056957],"study_design_scores_gemma":[0.00011597421,0.00024362675,0.13866751,0.00001612328,0.000031127616,0.00015666413,0.00016254581,0.79199183,0.06609412,0.0019284791,0.00054647215,0.00004555874],"about_ca_topic_score_codex":0.022540178,"about_ca_topic_score_gemma":0.009358777,"teacher_disagreement_score":0.022540178,"about_ca_system_score_codex":0.00089691195,"about_ca_system_score_gemma":0.00028856684,"threshold_uncertainty_score":0.044817984},"labels":[],"label_agreement":null},{"id":"W1637942467","doi":"10.1002/jgrb.50194","title":"The role of viscous magma mush spreading in volcanic flank motion at Kīlauea Volcano, Hawai‘i","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Space Agency; University of the Pacific; University of Hawai'i; U.S. Geological Survey; National Aeronautics and Space Administration; National Science Foundation","keywords":"Geology; Volcano; Magma; Flank; Dike; Seismology; Rift zone; Magma chamber; Geodesy; Interferometric synthetic aperture radar; Tectonics; Rift; Petrology; Synthetic aperture radar","score_opus":0.020674281772382862,"score_gpt":0.28080833577406217,"score_spread":0.2601340540016793,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1637942467","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972554,0.00009403092,0.0010980609,0.00009773157,0.0000067361957,0.0000063011457,0.00005457841,0.00002574313,0.001361348],"genre_scores_gemma":[0.9996897,0.000024936027,0.0001327845,0.0000056002004,0.0000021081378,0.0000020515367,0.000015684058,0.0000027689657,0.00012429857],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99997354,0.0000048307866,0.00000195241,0.000007583705,0.0000041994945,0.000007978715],"domain_scores_gemma":[0.9999006,0.000030497013,0.000023141658,0.000006953583,0.000013399472,0.000025440535],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011187188,0.00043606246,0.00023777988,0.00032399013,0.00040460375,0.000658511,0.00053669827,0.0005826567,0.0011926038],"category_scores_gemma":[0.00037947338,0.00029538656,0.00045903344,0.0001677047,0.00052827015,0.000537186,0.00028457656,0.0002549449,0.00012599683],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018568277,0.00014551893,0.22359775,0.000104328494,0.00016346021,0.0011945168,0.000428325,0.71623087,0.048000216,0.0022476779,0.00044982848,0.0072518196],"study_design_scores_gemma":[0.000038508475,0.000074886004,0.09260074,0.000015588832,0.00004122599,0.00007608102,0.00016216384,0.904546,0.0016383288,0.0005006176,0.00027644832,0.000029358462],"about_ca_topic_score_codex":0.046459213,"about_ca_topic_score_gemma":0.022183416,"teacher_disagreement_score":0.046459213,"about_ca_system_score_codex":0.0011605778,"about_ca_system_score_gemma":0.00046006395,"threshold_uncertainty_score":0.09237754},"labels":[],"label_agreement":null},{"id":"W1640721238","doi":"10.1002/jgrb.50345","title":"Semiautomated tremor detection using a combined cross‐correlation and neural network approach","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismology and Earthquake Studies","field":"Computer Science","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Computer science; Data set; Envelope (radar); Pattern recognition (psychology); Set (abstract data type); Event (particle physics); Waveform; Artificial intelligence; Noise (video); Data mining; Algorithm; Image (mathematics)","score_opus":0.04551331869360762,"score_gpt":0.33488404262728266,"score_spread":0.289370723933675,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1640721238","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.14635281,0.00020889698,0.8474966,0.00013628336,0.00004884166,0.00010467062,0.00021796346,0.0029628642,0.00247111],"genre_scores_gemma":[0.56225085,0.000119216835,0.43417057,0.000100835765,0.000052428175,0.00010367749,0.00077539816,0.0001519537,0.0022751142],"study_design_codex":"design_other","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9992106,0.00014570057,0.00005843932,0.00023301966,0.00026886215,0.00008333379],"domain_scores_gemma":[0.99795616,0.0006672442,0.00028574702,0.0002136492,0.0008186434,0.000058569534],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001182241,0.0008676726,0.0006010678,0.002490835,0.00031290832,0.0010028497,0.0008900224,0.0005576565,0.00080488244],"category_scores_gemma":[0.0027926578,0.00048318377,0.00066487363,0.001547125,0.00031374712,0.00083056133,0.0008476134,0.00058770203,0.00041398726],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032630577,0.0003952595,0.017878385,0.00013550477,0.0002979722,0.00023026255,0.00014759587,0.22406371,0.0639862,0.0010521854,0.0020973182,0.6893893],"study_design_scores_gemma":[0.000008210974,0.000038143906,0.00629665,0.000005444245,0.000018800072,0.00004444186,0.000017112372,0.9865522,0.006259264,0.00036745382,0.00037706294,0.000015154825],"about_ca_topic_score_codex":0.008150858,"about_ca_topic_score_gemma":0.013661802,"teacher_disagreement_score":0.008150858,"about_ca_system_score_codex":0.00051184645,"about_ca_system_score_gemma":0.00081640854,"threshold_uncertainty_score":0.016206801},"labels":[],"label_agreement":null},{"id":"W1838959485","doi":"10.1002/2013jb010739","title":"Hysteresis and coercivity of hematite","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":153,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; University of Minnesota; W. M. Keck Foundation; Earth Sciences Division; National Science Foundation","keywords":"Coercivity; Remanence; Magnetocrystalline anisotropy; Materials science; Hematite; Condensed matter physics; Saturation (graph theory); Magnetic anisotropy; Hysteresis; Nucleation; Magnetization; Anisotropy; Nuclear magnetic resonance; Chemistry; Metallurgy; Magnetic field; Physics; Optics","score_opus":0.02261457359285125,"score_gpt":0.3203741402916741,"score_spread":0.29775956669882286,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1838959485","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974764,0.000267809,0.000726739,0.000015711872,0.0000046862788,0.0000034888494,0.0001289238,0.00005255207,0.0013236486],"genre_scores_gemma":[0.9990802,0.000044358858,0.0001946609,0.0000031043953,0.0000017702706,0.0000021528203,0.00010328321,0.0000048433653,0.00056556624],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99994016,0.000005268356,0.0000024795406,0.000017720487,0.000022373808,0.000011889453],"domain_scores_gemma":[0.9998048,0.000047492365,0.000037592778,0.000011884828,0.00006262348,0.00003575076],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000080814905,0.000109690336,0.000061019902,0.00018558002,0.00009336745,0.00012953371,0.00010080028,0.00005146989,0.0010842739],"category_scores_gemma":[0.00022580138,0.00006470854,0.0000412958,0.00010650146,0.00016385701,0.000077203804,0.00007539308,0.00014379964,0.00010941694],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007595368,0.0000073261076,0.0026851536,0.000021834849,0.000004631415,0.000029932664,0.000043723103,0.000048985487,0.99455607,0.000089153196,0.000043879914,0.002393303],"study_design_scores_gemma":[0.0000046084892,0.00007180408,0.033258732,0.0000046031214,0.0000080632435,0.00012216931,0.000037786634,0.0012266572,0.9643619,0.00005451877,0.0008449163,0.0000042228817],"about_ca_topic_score_codex":0.001769726,"about_ca_topic_score_gemma":0.0013918047,"teacher_disagreement_score":0.001769726,"about_ca_system_score_codex":0.000268457,"about_ca_system_score_gemma":0.00011830122,"threshold_uncertainty_score":0.0036272407},"labels":[],"label_agreement":null},{"id":"W1842190251","doi":"10.1002/2015jb012112","title":"Magmatic expressions of continental lithosphere removal","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Dalhousie University","keywords":"Lithosphere; Geology; Magmatism; Asthenosphere; Lithospheric flexure; Craton; Delamination (geology); Crust; Geophysics; Obduction; Collision zone; Petrology; Seismology; Oceanic crust; Tectonics; Subduction","score_opus":0.060665723147725094,"score_gpt":0.3230612750957251,"score_spread":0.26239555194799996,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1842190251","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9407064,0.0008164969,0.028019821,0.00067981833,0.00003932911,0.000018026367,0.00061039376,0.0003199914,0.028789714],"genre_scores_gemma":[0.99804914,0.0000986809,0.0006833702,0.0000134872225,0.000011894036,0.000004544185,0.00009578438,0.000018258379,0.001024852],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99991417,0.000012375647,0.000007035417,0.00001736644,0.000026085061,0.000022970378],"domain_scores_gemma":[0.9995952,0.00012350321,0.00011806526,0.000043676737,0.000090913614,0.000028585802],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000197887,0.00030187747,0.00014730488,0.0009261029,0.0002779904,0.0005234952,0.00055976294,0.00036929536,0.0016633676],"category_scores_gemma":[0.0018795067,0.0002124846,0.0005638846,0.0005255505,0.0005083995,0.0004240919,0.00047552763,0.00033030257,0.00017010565],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007862055,0.000027302485,0.048334673,0.00015858645,0.00008385444,0.000604279,0.0002311364,0.8164898,0.03419695,0.085898906,0.00067442964,0.013221472],"study_design_scores_gemma":[0.000015378706,0.000019960296,0.033513743,0.00001398447,0.000024103916,0.00022308376,0.00005837146,0.94178534,0.006040384,0.01632976,0.0019535888,0.00002239527],"about_ca_topic_score_codex":0.005762005,"about_ca_topic_score_gemma":0.003425615,"teacher_disagreement_score":0.005762005,"about_ca_system_score_codex":0.0012962926,"about_ca_system_score_gemma":0.0002591355,"threshold_uncertainty_score":0.011456966},"labels":[],"label_agreement":null},{"id":"W1851392737","doi":"10.1002/2013jb010351","title":"Shallow, old, and hydrologically insignificant fault zones in the Appalachian orogen","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Université du Québec à Montréal; Natural Sciences and Engineering Research Council of Canada; Canadian Institute for Advanced Research","keywords":"Groundwater; Geology; Aquifer; Bedrock; Groundwater flow; Thrust fault; Paleozoic; Fault (geology); Hydrology (agriculture); Permeability (electromagnetism); Geochemistry; Petrology; Geomorphology; Geotechnical engineering; Seismology","score_opus":0.041507577070985145,"score_gpt":0.30242461695016987,"score_spread":0.26091703987918474,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1851392737","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99951696,0.000028131108,0.000040263185,0.0000073280594,2.967598e-7,0.00000270564,0.00007483771,0.0000020110906,0.0003275908],"genre_scores_gemma":[0.99976593,0.000031623713,0.00006464164,0.000003884765,5.2176085e-7,0.000002139336,0.000068023655,5.5301143e-7,0.00006265725],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984753,0.000023175811,0.000010022679,0.000040435985,0.000024289177,0.000054468903],"domain_scores_gemma":[0.9997949,0.000057422305,0.00006443006,0.000016040634,0.00004316959,0.000024036846],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016590474,0.00017372494,0.00021930652,0.00084855,0.000736138,0.0007896737,0.0003237021,0.00020325113,0.0006047172],"category_scores_gemma":[0.0004884099,0.00014027397,0.00016997367,0.0012681349,0.00083508866,0.00021373302,0.00037488746,0.0001257269,0.000041703228],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000121325575,0.000028273667,0.9838129,0.000039085848,0.00006453122,0.00059993914,0.0007532985,0.0036510574,0.0052017192,0.00030398418,0.00006747229,0.0053563807],"study_design_scores_gemma":[0.0000061897435,0.000015430864,0.99543554,0.0000078243975,0.000027940034,0.000076628996,0.0010525876,0.0027592925,0.000269369,0.0000978359,0.00024459828,0.0000068065306],"about_ca_topic_score_codex":0.57267666,"about_ca_topic_score_gemma":0.68502384,"teacher_disagreement_score":0.57267666,"about_ca_system_score_codex":0.002252921,"about_ca_system_score_gemma":0.0014340497,"threshold_uncertainty_score":0.8596799},"labels":[],"label_agreement":null},{"id":"W1887195454","doi":"10.1002/2014jb011727","title":"Influences on the positioning of mantle plumes following supercontinent formation","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"","keywords":"Supercontinent; Geology; Subduction; Mantle (geology); Mantle plume; Mantle convection; Hotspot (geology); Geophysics; Plate tectonics; Earth science; Craton; Geochemistry; Paleontology; Tectonics; Lithosphere","score_opus":0.06361993748045225,"score_gpt":0.3131089563955121,"score_spread":0.24948901891505987,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1887195454","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984561,0.00006768737,0.00060287345,0.000023111754,0.0000029292478,0.0000023461287,0.000045252822,0.000023545263,0.0007761828],"genre_scores_gemma":[0.9996357,0.000033361513,0.00018227637,0.0000034390912,0.0000010140623,0.0000016546544,0.000041173975,0.0000072698986,0.00009406284],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999231,0.000015197231,0.0000038996013,0.00001804647,0.000016130905,0.0000236033],"domain_scores_gemma":[0.99967396,0.00011616941,0.00006701623,0.000035693178,0.000046690373,0.000060549606],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017554277,0.00029184352,0.00026066342,0.0006548136,0.00038383532,0.0010802669,0.00038028634,0.00033627183,0.0011246214],"category_scores_gemma":[0.0011046082,0.00026569093,0.00056824356,0.00029600563,0.0004553083,0.00044254,0.00094227033,0.0003503918,0.00016013026],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003542916,0.00010679291,0.29466775,0.000101607504,0.00019243275,0.0008279493,0.00056820235,0.5705071,0.12000308,0.0023579772,0.0002536705,0.010059097],"study_design_scores_gemma":[0.00007934639,0.00024461863,0.29545394,0.000036176483,0.00012296456,0.00023214734,0.0006354123,0.68207026,0.018178128,0.0015299794,0.0013234947,0.00009358317],"about_ca_topic_score_codex":0.010377309,"about_ca_topic_score_gemma":0.0048698406,"teacher_disagreement_score":0.010377309,"about_ca_system_score_codex":0.00068435946,"about_ca_system_score_gemma":0.00034658302,"threshold_uncertainty_score":0.020633817},"labels":[],"label_agreement":null},{"id":"W1896307426","doi":"10.1002/jgrb.50118","title":"InSAR Evidence for an active shallow thrust fault beneath the city of Spokane Washington, USA","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismology; Geology; Interferometric synthetic aperture radar; Fault (geology); Seismic hazard; Seismic gap; Thrust fault; Active fault; Slip (aerodynamics); Synthetic aperture radar; Remote sensing; Engineering","score_opus":0.1691329890104908,"score_gpt":0.3888724245118331,"score_spread":0.21973943550134234,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1896307426","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9882533,0.00016970899,0.00022745488,0.0003766157,0.0000263531,0.000011746415,0.0026967255,0.000021012287,0.008217183],"genre_scores_gemma":[0.99547076,0.00021020218,0.00036289592,0.00012146302,0.000017434924,0.000009838368,0.0023867975,0.000004167039,0.0014164164],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998908,0.0000070560686,0.000007521383,0.00002550116,0.000029072957,0.00003997791],"domain_scores_gemma":[0.9996088,0.000026042226,0.000105841726,0.000034459998,0.00016011234,0.000064701286],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012695257,0.00019854355,0.000120469835,0.0009496504,0.00079998444,0.00064027734,0.00020664737,0.00034556867,0.0015249113],"category_scores_gemma":[0.0004650971,0.00014671571,0.00007669873,0.0012044212,0.00034908997,0.00024001936,0.0005099793,0.00034073764,0.00032851315],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008343697,0.00003648729,0.96587765,0.00007518316,0.00006589979,0.00066063745,0.0012343285,0.00021279651,0.0064209583,0.00022877663,0.00788398,0.01721986],"study_design_scores_gemma":[0.000003988395,0.000009270431,0.993386,0.000019282214,0.000012872216,0.000111634305,0.0015378254,0.0001304056,0.00031013525,0.000024595762,0.004448818,0.0000052338933],"about_ca_topic_score_codex":0.19362558,"about_ca_topic_score_gemma":0.4228378,"teacher_disagreement_score":0.19362558,"about_ca_system_score_codex":0.00050025765,"about_ca_system_score_gemma":0.0008508243,"threshold_uncertainty_score":0.38499707},"labels":[],"label_agreement":null},{"id":"W1898352123","doi":"10.1002/2014jb011011","title":"The peridotite ridge province in the southern Iberia Abyssal Plain: Seismic constraints revisited","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; Luonnontieteiden ja Tekniikan Tutkimuksen Toimikunta; Natural Environment Research Council; Sight Research UK","keywords":"Geology; Peridotite; Ridge; Seismology; Mantle (geology); Oceanic crust; Basement; Crust; Magnetic anomaly; Continental margin; Basalt; Paleontology; Tectonics; Subduction","score_opus":0.022680257245982105,"score_gpt":0.27596892829752356,"score_spread":0.25328867105154146,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1898352123","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9883123,0.0014552977,0.00027759536,0.0002749,0.000007288186,0.00000792034,0.00045414624,0.000014278942,0.009196287],"genre_scores_gemma":[0.9982748,0.00047769555,0.00034690354,0.00003610005,0.000014237444,0.000004916028,0.0004854484,0.0000034471934,0.00035640385],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981374,0.00003854323,0.000015320784,0.000047269255,0.000032805,0.000052361385],"domain_scores_gemma":[0.9996662,0.000069941445,0.00012639952,0.000019654484,0.00007055094,0.00004718522],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005147328,0.00027496723,0.00034996003,0.0025127756,0.00078861037,0.0021428189,0.000304681,0.00027511854,0.0029241976],"category_scores_gemma":[0.00068319566,0.00016859488,0.00016712301,0.0027469192,0.00057772984,0.00038095837,0.0009486809,0.00029888997,0.00027756375],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014934801,0.00006661889,0.94690704,0.000102682694,0.00012322768,0.00038823512,0.0011124479,0.0025091625,0.006816478,0.0022950338,0.00065820734,0.038871516],"study_design_scores_gemma":[0.000008548339,0.000010038716,0.99445987,0.00005806493,0.000018975958,0.00008900627,0.0010892269,0.001295471,0.00015720454,0.0003652448,0.0024440875,0.000004238528],"about_ca_topic_score_codex":0.08706677,"about_ca_topic_score_gemma":0.12505046,"teacher_disagreement_score":0.08706677,"about_ca_system_score_codex":0.0009664803,"about_ca_system_score_gemma":0.00087075646,"threshold_uncertainty_score":0.17311996},"labels":[],"label_agreement":null},{"id":"W1903059073","doi":"10.1002/jgrb.50101","title":"Heterogeneous rupture in the great Cascadia earthquake of 1700 inferred from coastal subsidence estimates","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":153,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Ocean Networks Canada Society; University of Victoria","funders":"U.S. Geological Survey; University of Victoria; National Science Foundation","keywords":"Geology; Subduction; Seismology; Slip (aerodynamics); Episodic tremor and slip; Moment magnitude scale; Plate tectonics; Subsidence; Tectonics; Paleontology; Geometry","score_opus":0.04319703663587497,"score_gpt":0.3080497416380789,"score_spread":0.2648527050022039,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1903059073","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984041,0.000057875946,0.00027225495,0.000014827641,0.000001486626,0.0000017841706,0.00038008858,0.000022728898,0.00084494986],"genre_scores_gemma":[0.9993783,0.000033723656,0.00011659548,0.000002635113,0.0000013208219,9.565798e-7,0.00040232058,0.0000026559098,0.000061342726],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988997,0.000016773123,0.000014326331,0.000031653344,0.000028115048,0.00001918549],"domain_scores_gemma":[0.999395,0.0001326192,0.00016926284,0.00008544283,0.00010848441,0.000109135566],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004296238,0.00043025677,0.00020584719,0.0015565271,0.00025477968,0.000695649,0.00032938216,0.0003343372,0.0010192688],"category_scores_gemma":[0.001524094,0.00036399427,0.0002923696,0.001110268,0.00032231663,0.00033747457,0.00051963044,0.0001629555,0.00029989498],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000042036656,0.00001132118,0.98783964,0.000024669622,0.000051552353,0.00012114025,0.00015697192,0.007093207,0.0019494898,0.00009657433,0.00015101371,0.0024623296],"study_design_scores_gemma":[0.0000031304878,0.000011106801,0.9920614,0.000007273259,0.0000124668895,0.00003953307,0.00012886347,0.007196618,0.0002342399,0.00006402645,0.00023381361,0.0000075019693],"about_ca_topic_score_codex":0.052295607,"about_ca_topic_score_gemma":0.06123678,"teacher_disagreement_score":0.052295607,"about_ca_system_score_codex":0.000862607,"about_ca_system_score_gemma":0.00034013786,"threshold_uncertainty_score":0.10398239},"labels":[],"label_agreement":null},{"id":"W1915783104","doi":"10.1002/2014jb011385","title":"Spatiotemporal changes, faulting regimes, and source parameters of induced seismicity: A case study from The Geysers geothermal field","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":136,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Lawrence Berkeley National Laboratory; Helmholtz-Alberta Initiative; Helmholtz-Gemeinschaft","keywords":"Induced seismicity; Geothermal gradient; Hypocenter; Geology; Pore water pressure; Poromechanics; Slip (aerodynamics); Injection well; Hydraulic fracturing; Seismology; Fault (geology); Hydrogeology; Petrology; Geotechnical engineering; Geophysics; Petroleum engineering","score_opus":0.067117975632054,"score_gpt":0.32099736891729513,"score_spread":0.2538793932852411,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1915783104","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994523,0.000016085327,0.00008041851,0.0000072950093,3.9365693e-7,0.000006091722,0.00015965657,0.000010055205,0.00026766653],"genre_scores_gemma":[0.9988649,0.000038493068,0.0004063308,0.0000031707425,0.000002084558,0.0000050093445,0.00041765065,0.0000029244281,0.00025936466],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990916,0.000011170136,0.0000061554183,0.000025452939,0.000024707528,0.000023288356],"domain_scores_gemma":[0.9997515,0.000068748086,0.00007737158,0.000025008518,0.00004539211,0.00003192345],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019789433,0.00022689623,0.00016169838,0.0011421046,0.00033374998,0.00029914483,0.00025991965,0.00024003447,0.0005389166],"category_scores_gemma":[0.00045534302,0.00011805894,0.00018620072,0.0010241542,0.00037960292,0.00018164607,0.00026952798,0.00013967202,0.000052996333],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002806868,0.00022124783,0.9217567,0.00011702709,0.00012340747,0.00774771,0.0023557267,0.02286586,0.021846522,0.00035172436,0.0010355678,0.021297844],"study_design_scores_gemma":[0.00001929647,0.00007547471,0.9877303,0.000009435,0.00003187433,0.0003245169,0.0010112986,0.00846281,0.0015962682,0.00004741975,0.00067769166,0.000013587929],"about_ca_topic_score_codex":0.10248698,"about_ca_topic_score_gemma":0.19921736,"teacher_disagreement_score":0.10248698,"about_ca_system_score_codex":0.0006800454,"about_ca_system_score_gemma":0.0004304383,"threshold_uncertainty_score":0.20378083},"labels":[],"label_agreement":null},{"id":"W1920914286","doi":"10.1002/jgrb.50181","title":"Annual modulation of non‐volcanic tremor in northern Cascadia","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Subduction; Seismology; Crust; Volcano; Shear (geology); Continental crust; Oceanic crust; Oceanography; Paleontology; Tectonics","score_opus":0.028777753506722164,"score_gpt":0.3020246454097679,"score_spread":0.27324689190304574,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1920914286","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9965642,0.00011709393,0.000051225292,0.00008281045,0.0000063308044,0.000004268764,0.0008294553,0.00004720846,0.002297437],"genre_scores_gemma":[0.99890447,0.000079014404,0.000030710857,0.000008311759,0.0000043101186,0.000004236423,0.0005984036,0.000005784134,0.00036483054],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984586,0.000012107835,0.000014598388,0.00005427364,0.00003534699,0.000037760616],"domain_scores_gemma":[0.9991779,0.000053605443,0.0002061787,0.000060134553,0.00018874029,0.00031344077],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018521708,0.00029686312,0.00024302305,0.001665242,0.0007389157,0.0006930573,0.00032522398,0.000268404,0.0021987183],"category_scores_gemma":[0.0010354015,0.00023010357,0.0002470347,0.0014236341,0.0004454247,0.00019960024,0.00075678725,0.0002161068,0.00032380302],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010625634,0.000026102462,0.98565036,0.00006863978,0.000100770856,0.00044825167,0.0013170748,0.0013692896,0.004023029,0.00009708467,0.0012043987,0.0055887555],"study_design_scores_gemma":[0.0000013071068,0.0000032301602,0.9992735,0.0000041270864,0.0000052609385,0.000019741328,0.000150273,0.00019798407,0.000029325114,0.000009503925,0.0003030296,0.0000027927367],"about_ca_topic_score_codex":0.3061396,"about_ca_topic_score_gemma":0.49335942,"teacher_disagreement_score":0.6938604,"about_ca_system_score_codex":0.0020280173,"about_ca_system_score_gemma":0.0010681933,"threshold_uncertainty_score":0.6087153},"labels":[],"label_agreement":null},{"id":"W1925025952","doi":"10.1002/2014jb011190","title":"Salinity‐buffered methane hydrate formation and dissociation in gas‐rich systems","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Penn West Exploration (Canada); University of Calgary","funders":"Geothermal Technologies Program; U.S. Department of Energy","keywords":"Hydrate; Clathrate hydrate; Methane; Nucleation; Dissociation (chemistry); Salinity; Natural gas; Chemistry; Brine; Thermodynamic equilibrium; Thermodynamics; Chemical physics; Geology; Physical chemistry","score_opus":0.05600093372475553,"score_gpt":0.3354426511756013,"score_spread":0.2794417174508458,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1925025952","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99866104,0.000049498198,0.0010543143,0.000011408268,0.0000015854596,0.0000037252778,0.0000321285,0.000022223287,0.00016404633],"genre_scores_gemma":[0.9997019,0.00001579319,0.00021188524,0.0000020910597,3.8689902e-7,0.0000020998364,0.00002509778,0.0000014275898,0.00003917476],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99992704,0.000011472458,0.0000064624155,0.000017636163,0.000021798762,0.000015614123],"domain_scores_gemma":[0.99991345,0.000025373021,0.000022014081,0.000009278052,0.000014826058,0.000015025205],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001156709,0.0001259454,0.00021387756,0.00016520181,0.00019068312,0.00028515395,0.00024710372,0.00016154966,0.00031975153],"category_scores_gemma":[0.00028440647,0.00013889694,0.00013916047,0.00009850586,0.00039977313,0.0003268702,0.0002807969,0.00020629833,0.000052801053],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011650865,0.000030957428,0.01088968,0.00005876828,0.00002416194,0.00012695813,0.000079067635,0.00925629,0.97747505,0.00055676734,0.000033411055,0.0013522964],"study_design_scores_gemma":[0.000036716654,0.00024877526,0.037007194,0.0000055429573,0.000018903142,0.00014155605,0.00016613133,0.15832575,0.8022379,0.00094595744,0.00083818176,0.000027326618],"about_ca_topic_score_codex":0.0026465217,"about_ca_topic_score_gemma":0.0025422995,"teacher_disagreement_score":0.0026465217,"about_ca_system_score_codex":0.0004688706,"about_ca_system_score_gemma":0.00019441584,"threshold_uncertainty_score":0.005262196},"labels":[],"label_agreement":null},{"id":"W1929992685","doi":"10.1002/2013jb010564","title":"Multifaulting in a tectonic syntaxis revealed by InSAR: The case of the Ziarat earthquake sequence (Pakistan)","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Safran Electronics (Canada)","funders":"","keywords":"Geology; Seismology; Sinistral and dextral; Interferometric synthetic aperture radar; Tectonics; Fault (geology); Strike-slip tectonics; Slip (aerodynamics); Shear (geology); Inversion (geology); Geodesy; Synthetic aperture radar; Petrology","score_opus":0.04142221945835021,"score_gpt":0.33755282019037486,"score_spread":0.29613060073202463,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1929992685","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99865973,0.00004563863,0.00015826024,0.00012187118,0.0000026699402,0.00000484462,0.00013206441,0.000005896771,0.0008690661],"genre_scores_gemma":[0.9996636,0.000025250849,0.00013901682,0.000006423434,0.0000026329433,0.0000011315651,0.00009867137,0.0000013814258,0.00006189359],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998217,0.000025431398,0.000009925693,0.000048905014,0.000032910204,0.00006122731],"domain_scores_gemma":[0.99964786,0.0000762233,0.00014326176,0.000041171337,0.000051912695,0.000039514045],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002994133,0.0002844206,0.00018987649,0.0010148905,0.00069381663,0.00097539916,0.00034311676,0.00055260374,0.001105723],"category_scores_gemma":[0.0011696061,0.00024697394,0.0001842555,0.0010549471,0.0009425176,0.0005335278,0.0004961572,0.00036929798,0.000186189],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00050305633,0.000110516776,0.8970483,0.000086378175,0.00018786814,0.035565093,0.0025537421,0.017274473,0.020569043,0.005346399,0.0017867974,0.018968368],"study_design_scores_gemma":[0.000041756244,0.00006457066,0.9646341,0.000027130316,0.00007934325,0.0021187812,0.0027797967,0.025956757,0.0015418357,0.00084587693,0.001878137,0.000031782838],"about_ca_topic_score_codex":0.0432609,"about_ca_topic_score_gemma":0.051088713,"teacher_disagreement_score":0.0432609,"about_ca_system_score_codex":0.0009991213,"about_ca_system_score_gemma":0.0003503302,"threshold_uncertainty_score":0.086018205},"labels":[],"label_agreement":null},{"id":"W1930176674","doi":"10.1002/2015jb012209","title":"Magnitude and symmetry of seismic anisotropy in mica‐ and amphibole‐bearing metamorphic rocks and implications for tectonic interpretation of seismic data from the southeast Tibetan Plateau","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":115,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Bedford Institute of Oceanography; Polytechnique Montréal","funders":"Centre of Excellence for Core to Crust Fluid Systems, Australian Research Council; Natural Sciences and Engineering Research Council of Canada","keywords":"Schist; Geology; Amphibole; Metamorphic rock; Mica; Gneiss; Muscovite; Crenulation; Geochemistry; Petrology; Seismology; Quartz; Tectonics; Shear zone","score_opus":0.07223117621662183,"score_gpt":0.3364663469106367,"score_spread":0.26423517069401486,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1930176674","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985556,0.000033050175,0.0005205166,0.00001710978,0.0000015516038,0.0000035606336,0.00019874978,0.000027086207,0.00064282824],"genre_scores_gemma":[0.99936014,0.000010841843,0.00030465025,0.0000023947916,0.0000015374391,0.0000015887317,0.00025770304,0.0000060481575,0.000055197266],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99978906,0.00005609853,0.000024084939,0.000050286446,0.000052206968,0.00002831506],"domain_scores_gemma":[0.99940073,0.0000953041,0.00015935687,0.00006386149,0.00022211208,0.000058583093],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007990474,0.0002636809,0.00017824615,0.0021100973,0.00023555926,0.0006415313,0.00020994394,0.00017509994,0.0011091491],"category_scores_gemma":[0.0016987126,0.00019949788,0.00016253744,0.0012452181,0.00023750526,0.00017987563,0.00025514822,0.00015282589,0.00019288588],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019864838,0.000028970653,0.90739,0.000032397977,0.00003944603,0.00013940224,0.00032140018,0.0045584394,0.06273891,0.00018587631,0.00011736127,0.024249133],"study_design_scores_gemma":[0.000007957237,0.000020000332,0.9920644,0.0000046211253,0.000005253507,0.00006822964,0.00010282597,0.0063655013,0.0011932068,0.00006055432,0.00010312738,0.000004429296],"about_ca_topic_score_codex":0.01113594,"about_ca_topic_score_gemma":0.011292124,"teacher_disagreement_score":0.01113594,"about_ca_system_score_codex":0.00037238377,"about_ca_system_score_gemma":0.0002219814,"threshold_uncertainty_score":0.022142231},"labels":[],"label_agreement":null},{"id":"W1930401817","doi":"10.1002/jgrb.50100","title":"Waveform tomography in 2.5D: Parameterization for crooked‐line acquisition geometry","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Waveform; Tomography; Geology; Inversion (geology); Attenuation; Seismology; Seismic tomography; Refraction; Reflection (computer programming); Acoustics; Geometry; Geodesy; Computer science; Optics; Physics; Telecommunications; Mathematics","score_opus":0.039930106022840806,"score_gpt":0.3155376699763248,"score_spread":0.275607563953484,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1930401817","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.042287342,0.00002665797,0.953747,0.00005808194,0.000016693939,0.00007016283,0.00046785953,0.0015670635,0.0017592038],"genre_scores_gemma":[0.55636466,0.000090337024,0.43983424,0.00005060339,0.000011129753,0.00022544328,0.0013872876,0.00056336296,0.0014729026],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99984026,0.000038451588,0.000013112372,0.000023271721,0.000066662935,0.000018198667],"domain_scores_gemma":[0.9995547,0.00017123348,0.000055171382,0.00007710873,0.0001258334,0.000015952686],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035775147,0.00062815176,0.00026784645,0.00059538434,0.00018598302,0.00080618163,0.0009164307,0.0005184895,0.0030564812],"category_scores_gemma":[0.0016859946,0.00039121875,0.00044744083,0.0005231924,0.00025486617,0.0004774525,0.00059873663,0.00050583325,0.0005410606],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005360931,0.00004472119,0.0027653917,0.000049840917,0.000019006051,0.00020380008,0.00008151393,0.9250404,0.016909428,0.004670871,0.0013290069,0.048832405],"study_design_scores_gemma":[0.000003434138,0.0000043406358,0.00027330554,0.0000021874807,0.0000011213035,0.000025746556,0.000007634679,0.9965372,0.0020523688,0.00023479795,0.00085173035,0.0000061670403],"about_ca_topic_score_codex":0.01201023,"about_ca_topic_score_gemma":0.010153336,"teacher_disagreement_score":0.01201023,"about_ca_system_score_codex":0.0005036946,"about_ca_system_score_gemma":0.00079705875,"threshold_uncertainty_score":0.0238806},"labels":[],"label_agreement":null},{"id":"W1936698890","doi":"10.1002/jgrb.50352","title":"A new calibration of seismic velocities, anisotropy, fabrics, and elastic moduli of amphibole‐rich rocks","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":95,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Bedford Institute of Oceanography; Polytechnique Montréal","funders":"","keywords":"Amphibole; Geology; Peridotite; Mafic; Gneiss; Gabbro; Plagioclase; Petrology; Geochemistry; Mineralogy; Igneous rock; Basalt; Quartz; Metamorphic rock","score_opus":0.020930141843029097,"score_gpt":0.26859670691990023,"score_spread":0.24766656507687113,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1936698890","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9863115,0.00016257679,0.011942679,0.000012934751,0.000004411618,0.00001183372,0.0003128888,0.00018580048,0.0010552824],"genre_scores_gemma":[0.9918995,0.000082504856,0.007466161,0.000005641873,0.000004199427,0.000013254124,0.00026431205,0.000017176926,0.0002472231],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99976593,0.000032306936,0.00001334989,0.00007304753,0.00009946825,0.000015876565],"domain_scores_gemma":[0.99958545,0.00008994667,0.00013241683,0.000054775155,0.00011178245,0.000025699643],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033346153,0.0004950719,0.00018891973,0.0012867459,0.00015752275,0.0002478971,0.00035162998,0.00021470505,0.0010439841],"category_scores_gemma":[0.0010308026,0.00034015832,0.00012442489,0.000641931,0.00023769328,0.00041278356,0.00032106505,0.00028267477,0.00030076483],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010896619,0.00004983795,0.16274427,0.00005485182,0.000053188796,0.000076405544,0.00009956402,0.002784305,0.79836416,0.00017635182,0.00011299687,0.035375096],"study_design_scores_gemma":[0.000017086553,0.00017927923,0.5450887,0.000018416164,0.00004592506,0.00063999044,0.00015760571,0.033990055,0.4179322,0.00031529248,0.0015796854,0.0000357953],"about_ca_topic_score_codex":0.00080914964,"about_ca_topic_score_gemma":0.0012627172,"teacher_disagreement_score":0.0012867459,"about_ca_system_score_codex":0.00015215558,"about_ca_system_score_gemma":0.00010694517,"threshold_uncertainty_score":0.0034924746},"labels":[],"label_agreement":null},{"id":"W1945607800","doi":"10.1002/2013jb010535","title":"Ambient seismic noise tomography of Canada and adjacent regions: Part I. Crustal structures","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta; University of Victoria; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada; Royal Society Te Apārangi; Royal Society; Marsden Fund; National Science Foundation","keywords":"Geology; Crust; Mantle (geology); Seismology; Transition zone; Craton; Continental crust; Seismic tomography; Shield; Receiver function; Shear velocity; Velocity gradient; Seismometer; Geophysics; Petrology; Lithosphere; Tectonics","score_opus":0.01958870606416186,"score_gpt":0.2573237911233822,"score_spread":0.23773508505922036,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1945607800","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99254674,0.00031218774,0.0008132643,0.00004729143,0.0000046807713,0.000016583985,0.0027788065,0.000044019296,0.0034364439],"genre_scores_gemma":[0.996905,0.00019791191,0.00077528117,0.000012342523,0.000002656745,0.0000050856615,0.0013659954,0.000010514717,0.0007252955],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981576,0.0000061238356,0.000005104462,0.000029643239,0.00008313953,0.00006018936],"domain_scores_gemma":[0.9996636,0.0000122290185,0.00003824527,0.000010859168,0.00023136253,0.00004370656],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012215816,0.00036741435,0.00019913509,0.0019506485,0.0008285393,0.0008962742,0.00047265162,0.00018186787,0.00072230067],"category_scores_gemma":[0.0004874413,0.00019440954,0.00023371162,0.0040437714,0.0003520865,0.00024018466,0.00058167096,0.00023412288,0.00011990873],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020847475,0.000050422033,0.9082817,0.00008455996,0.0001780844,0.0007664134,0.0011309743,0.008410371,0.026455084,0.00075510313,0.0015194999,0.052159306],"study_design_scores_gemma":[0.000006201386,0.000010336584,0.99097556,0.000016299055,0.000026821928,0.00009798954,0.00048761498,0.004981612,0.001272138,0.00006073983,0.002051542,0.000013151141],"about_ca_topic_score_codex":0.9715469,"about_ca_topic_score_gemma":0.982064,"teacher_disagreement_score":0.028453112,"about_ca_system_score_codex":0.0057944064,"about_ca_system_score_gemma":0.0067460285,"threshold_uncertainty_score":0.05724132},"labels":[],"label_agreement":null},{"id":"W1945774637","doi":"10.1002/2013jb010929","title":"Feeding the “aneurysm”: Orogen‐parallel mass transport into Nanga Parbat and the western Himalayan syntaxis","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Crust; Tectonics; Shear zone; Massif; Transpression; Thickening; Shear (geology); Wedge (geometry); Terrane; Seismology; Geomorphology; Petrology; Geophysics; Paleontology; Geometry","score_opus":0.02225456345039404,"score_gpt":0.2693614335700013,"score_spread":0.24710687011960727,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1945774637","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9953825,0.000028803506,0.0012820454,0.000120911725,0.0000067499177,0.000004641487,0.00002495571,0.00003123918,0.0031180931],"genre_scores_gemma":[0.9994254,0.000017524097,0.0002173819,0.000008994449,0.0000025513427,0.0000019831693,0.000010292674,0.0000030214035,0.00031287147],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99997306,0.0000053997164,0.0000013373701,0.0000070632886,0.000003506763,0.000009720316],"domain_scores_gemma":[0.999966,0.000006389136,0.000009395793,0.00000402142,0.000004930903,0.000009312766],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000057162455,0.00027715942,0.00019684125,0.00021082255,0.0005720793,0.0006918632,0.00035646156,0.00045869075,0.0018083027],"category_scores_gemma":[0.00021457204,0.00023294009,0.00021348578,0.00017386928,0.00050076883,0.00033645876,0.0004958884,0.00024213493,0.00012285767],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004871697,0.00024085927,0.13187963,0.00015622855,0.00019330566,0.004552042,0.0008028169,0.70264727,0.110494606,0.03172031,0.0013596311,0.015466068],"study_design_scores_gemma":[0.00009939007,0.00016535536,0.06531731,0.000016414437,0.000052236464,0.0003747556,0.0005366952,0.92317104,0.0041814405,0.004896102,0.0011536677,0.000035635156],"about_ca_topic_score_codex":0.02681141,"about_ca_topic_score_gemma":0.014400936,"teacher_disagreement_score":0.02681141,"about_ca_system_score_codex":0.0010028129,"about_ca_system_score_gemma":0.00050087675,"threshold_uncertainty_score":0.053310752},"labels":[],"label_agreement":null},{"id":"W1948793628","doi":"10.1002/jgrb.50293","title":"Sea level variations during snowball Earth formation: 1. A preliminary analysis","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Snowball Earth; Geology; Freeboard; Sea level; Lithosphere; Sedimentary rock; Paleontology; Oceanography; Glacial period; Tectonics","score_opus":0.056150950648414,"score_gpt":0.3203961450697468,"score_spread":0.26424519442133276,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1948793628","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976827,0.00004004479,0.00015881553,0.000008613985,0.000002337489,0.0000042557695,0.0010541126,0.000009479253,0.0010396406],"genre_scores_gemma":[0.9974751,0.000030077803,0.00014772979,0.0000048780016,0.0000030382978,0.000003931317,0.0020159476,0.0000027235283,0.0003165407],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996424,0.0000029214214,0.0000035740247,0.000009177652,0.000007353543,0.000012714777],"domain_scores_gemma":[0.9998982,0.000015997255,0.00002187193,0.0000060887696,0.000032285858,0.000025644069],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000105209125,0.00017824513,0.00012074563,0.00070345943,0.00027949404,0.0003110568,0.00015484764,0.0001734988,0.0016205219],"category_scores_gemma":[0.00023208151,0.000053417214,0.00022327517,0.0006136137,0.00011035917,0.00019352439,0.00023604037,0.00013816434,0.00032953545],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048501723,0.000029017034,0.97636527,0.000027455437,0.000035269313,0.00021964758,0.00033599362,0.0010503879,0.012463474,0.0001637574,0.00026470915,0.008560055],"study_design_scores_gemma":[0.0000018945975,0.000040481442,0.99818975,0.0000014159343,0.000005377446,0.00001603192,0.000071929404,0.0005358715,0.00071623706,0.000018825385,0.000400699,0.0000016154878],"about_ca_topic_score_codex":0.017762428,"about_ca_topic_score_gemma":0.036694527,"teacher_disagreement_score":0.017762428,"about_ca_system_score_codex":0.00030069202,"about_ca_system_score_gemma":0.00015853882,"threshold_uncertainty_score":0.035318077},"labels":[],"label_agreement":null},{"id":"W1952808813","doi":"10.1002/2013jb010661","title":"Antigorite‐induced seismic anisotropy and implications for deformation in subduction zones and the Tibetan Plateau","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Bedford Institute of Oceanography; Polytechnique Montréal","funders":"China Geological Survey; Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Subduction; Shear wave splitting; Slab; Lithosphere; Seismic anisotropy; Trench; Seismology; Anisotropy; Mantle (geology); Shear (geology); Petrology; Crust; Mantle wedge; Geophysics; Tectonics","score_opus":0.03164634874895272,"score_gpt":0.3132510682928685,"score_spread":0.28160471954391575,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1952808813","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99921334,0.00013910842,0.00011187849,0.000028138496,0.0000013916493,0.0000013147292,0.00006486866,0.000007137265,0.00043275484],"genre_scores_gemma":[0.9998424,0.000040179577,0.000029139943,0.000003785692,0.0000021570202,7.147847e-7,0.000044977452,0.0000011040014,0.000035507557],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999192,0.000014892945,0.000010279449,0.000023851027,0.000015886542,0.00001596689],"domain_scores_gemma":[0.9997445,0.000042965014,0.00010275239,0.000021134825,0.000043372835,0.00004526452],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037371687,0.0003212564,0.00018937781,0.001428039,0.00035095215,0.0008138349,0.00027516784,0.00028479396,0.0010484114],"category_scores_gemma":[0.0005935472,0.00016111277,0.00019621034,0.0012074274,0.0006724803,0.0003985351,0.00045752435,0.00021272706,0.00011265828],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030048037,0.0000556878,0.9199125,0.00008066337,0.00006651154,0.0005938543,0.00049766543,0.0032432668,0.064757034,0.00045314882,0.000059017737,0.009980109],"study_design_scores_gemma":[0.0000054155043,0.000023034767,0.9966574,0.0000068080126,0.000006146164,0.00007736676,0.00022695313,0.002170615,0.0005328892,0.00019769205,0.00009111644,0.000004521864],"about_ca_topic_score_codex":0.009783396,"about_ca_topic_score_gemma":0.007128445,"teacher_disagreement_score":0.009783396,"about_ca_system_score_codex":0.00044526215,"about_ca_system_score_gemma":0.00027404077,"threshold_uncertainty_score":0.01945287},"labels":[],"label_agreement":null},{"id":"W1958905693","doi":"10.1002/2013jb010484","title":"The impact of Rayleigh number on assessing the significance of supercontinent insulation","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; University of Toronto; Government of Ontario; Compute Canada","keywords":"Mantle (geology); Subduction; Geology; Hotspot (geology); Supercontinent; Mantle convection; Geophysics; Continental margin; Earth science; Paleontology; Tectonics; Craton","score_opus":0.03483319028969537,"score_gpt":0.36566625384661283,"score_spread":0.33083306355691744,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1958905693","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99636626,0.00016272032,0.0013167657,0.00017467118,0.000012907978,0.000008358358,0.000058337806,0.000050260267,0.0018496758],"genre_scores_gemma":[0.99919385,0.000051407405,0.00056688883,0.000018981236,0.0000058998967,0.0000037065113,0.000028164313,0.000025212641,0.000105758954],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99961925,0.00017440882,0.000020705389,0.00005257384,0.0000491209,0.0000838997],"domain_scores_gemma":[0.9963862,0.002630266,0.0002848978,0.00025585026,0.00015075887,0.00029205394],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011269534,0.0010417228,0.0006155144,0.0007993981,0.00064584584,0.001543625,0.0009826664,0.0010366752,0.0012876801],"category_scores_gemma":[0.0077088843,0.00037048353,0.0009445498,0.00053075305,0.0018301759,0.0014265556,0.0014837381,0.00096373004,0.000121596946],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041616702,0.00013225463,0.11861239,0.000104632905,0.0002773452,0.00057008606,0.00033996845,0.8562954,0.013851552,0.0036744531,0.00033141114,0.0053943377],"study_design_scores_gemma":[0.000060864524,0.00020387521,0.028315092,0.00003424567,0.0000962974,0.00010480723,0.0002596239,0.96403915,0.004588168,0.0019041963,0.00034485225,0.000048794816],"about_ca_topic_score_codex":0.013580215,"about_ca_topic_score_gemma":0.006558067,"teacher_disagreement_score":0.013580215,"about_ca_system_score_codex":0.0005450969,"about_ca_system_score_gemma":0.0005819807,"threshold_uncertainty_score":0.027002335},"labels":[],"label_agreement":null},{"id":"W1960489672","doi":"10.1002/2014jb011842","title":"Indentor‐corner tectonics in the Yakutat‐St. Elias collision constrained by GPS","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary; University of Victoria","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; Agence Nationale de la Recherche","keywords":"Geology; Seismology; Transpression; Geodesy; Tectonics; Plate tectonics; Strain rate; Fault (geology); Shear zone; Physics","score_opus":0.0735861886388752,"score_gpt":0.34223329595287827,"score_spread":0.2686471073140031,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1960489672","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990852,0.000023010598,0.000033431945,0.000010013069,8.12809e-7,0.0000017558365,0.00022885713,0.00000404051,0.00061289605],"genre_scores_gemma":[0.9992994,0.00001912903,0.00006751178,0.0000024476797,7.3759844e-7,0.000001969309,0.0003682777,0.0000016740729,0.00023886455],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998671,0.000015642383,0.000006784404,0.00003619096,0.000029344745,0.000044996756],"domain_scores_gemma":[0.9997558,0.000034028726,0.000073927295,0.000021283304,0.000068249166,0.000046717803],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015110792,0.00015364017,0.00024089654,0.0010164159,0.0005864263,0.00086727296,0.00030791768,0.00020193758,0.0011696841],"category_scores_gemma":[0.00062178884,0.00015144228,0.00011640517,0.0017416915,0.00028172878,0.00021379886,0.00074421545,0.00018583288,0.00012778732],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000070975235,0.000016648906,0.9924585,0.0000060256607,0.000019532787,0.00016179396,0.0005666272,0.0021142694,0.0012307942,0.00010897777,0.00014482455,0.0031010392],"study_design_scores_gemma":[0.0000031862585,0.0000059710164,0.99715143,0.0000066852385,0.000005794454,0.000025561309,0.00075948157,0.0015890212,0.00008800248,0.00002651153,0.0003343568,0.000004025907],"about_ca_topic_score_codex":0.36902905,"about_ca_topic_score_gemma":0.61272067,"teacher_disagreement_score":0.36902905,"about_ca_system_score_codex":0.0014648429,"about_ca_system_score_gemma":0.0009881463,"threshold_uncertainty_score":0.73376215},"labels":[],"label_agreement":null},{"id":"W1977954145","doi":"10.1002/2014jb011492","title":"Geodetic imaging of potential seismogenic asperities on the Xianshuihe‐Anninghe‐Zemuhe fault system, southwest China, with a new 3‐D viscoelastic interseismic coupling model","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":130,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"China Postdoctoral Science Foundation; National Natural Science Foundation of China","keywords":"Geology; Viscoelasticity; Seismology; Geodesy; Asperity (geotechnical engineering); Slip (aerodynamics); Interferometric synthetic aperture radar; Geodetic datum; Crust; Synthetic aperture radar; Remote sensing; Geophysics; Materials science; Geotechnical engineering; Physics","score_opus":0.04316034868720262,"score_gpt":0.2867110519182586,"score_spread":0.24355070323105596,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1977954145","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9961516,0.000027998876,0.0033228758,0.000032665364,0.0000022661675,0.0000064520973,0.000099577905,0.00005114742,0.0003053463],"genre_scores_gemma":[0.9972366,0.000024795494,0.0024618085,0.0000054223583,0.0000023855546,0.00000395015,0.000108885535,0.0000029126859,0.00015318798],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999536,0.0000055567293,0.0000025530198,0.000016142492,0.000012365458,0.000009805484],"domain_scores_gemma":[0.99993885,0.0000063161074,0.000015256719,0.000013151312,0.000010458316,0.000015907426],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001320241,0.00032092916,0.00017835615,0.0007130315,0.00017666325,0.00029058303,0.00031168107,0.00028960672,0.00038128573],"category_scores_gemma":[0.00015526755,0.00026748283,0.0003299677,0.00046236135,0.00018503053,0.00023665896,0.00029737328,0.00016209079,0.000062751715],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034031674,0.0002305092,0.29999408,0.00008950539,0.00021367763,0.00049571646,0.0004895988,0.47310555,0.16560982,0.0007336957,0.00048657393,0.0582109],"study_design_scores_gemma":[0.000026564234,0.00005417987,0.15408263,0.00000478244,0.000032118885,0.000042117656,0.00006796929,0.84230226,0.0030346757,0.00010446123,0.00022900292,0.000019319146],"about_ca_topic_score_codex":0.02101796,"about_ca_topic_score_gemma":0.031625792,"teacher_disagreement_score":0.02101796,"about_ca_system_score_codex":0.00053641264,"about_ca_system_score_gemma":0.00051932194,"threshold_uncertainty_score":0.04179126},"labels":[],"label_agreement":null},{"id":"W1983183835","doi":"10.1002/2014jb011430","title":"Tidal modulation and triggering of low‐frequency earthquakes in northern Cascadia","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":77,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Geology; Slip (aerodynamics); Seismology; Shear (geology); Shear stress; Episodic tremor and slip; Low frequency; Tidal force; Subduction; Petrology; Mechanics; Tectonics; Physics","score_opus":0.028395886563947603,"score_gpt":0.29313937714228266,"score_spread":0.2647434905783351,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1983183835","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99906963,0.000037016336,0.000030629522,0.000023750696,0.0000012223787,0.0000019248166,0.00042517993,0.000010518452,0.0004001298],"genre_scores_gemma":[0.99943155,0.00002727932,0.000017557813,0.0000028222628,0.0000014527044,0.0000019291401,0.0003846594,0.000001972534,0.00013079858],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998056,0.00003070484,0.000018239387,0.000056427896,0.00004668713,0.000042338303],"domain_scores_gemma":[0.9985714,0.00021341893,0.00046443765,0.00013330742,0.00027966895,0.00033774562],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003537735,0.00024993523,0.000282946,0.0016421129,0.0004428099,0.0006309863,0.00023994363,0.00020370433,0.0013090159],"category_scores_gemma":[0.0018819099,0.00019421964,0.0002743644,0.0016398317,0.0004172046,0.0002206217,0.0006828705,0.00019836873,0.00020297126],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005443162,0.000010832296,0.9945846,0.000015903168,0.000057225072,0.00013579625,0.00039347776,0.0008270052,0.0015457728,0.000021829937,0.00017536992,0.0021777747],"study_design_scores_gemma":[7.2445744e-7,0.0000036531906,0.9995722,0.0000014756228,0.0000038805842,0.000010268252,0.00009536637,0.00020826253,0.0000344167,0.000005334603,0.000062928455,0.0000015627177],"about_ca_topic_score_codex":0.21871586,"about_ca_topic_score_gemma":0.34861365,"teacher_disagreement_score":0.78128415,"about_ca_system_score_codex":0.001169669,"about_ca_system_score_gemma":0.0005956946,"threshold_uncertainty_score":0.43488556},"labels":[],"label_agreement":null},{"id":"W1986739614","doi":"10.1002/2014jb011262","title":"Retrieving surface waves from ambient seismic noise using seismic interferometry by multidimensional deconvolution","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Netherlands Research Centre for Integrated Solid Earth Sciences; National Science Foundation","keywords":"Deconvolution; Seismic interferometry; Ambient noise level; Rayleigh wave; Noise (video); Geology; Acoustics; Seismic noise; Cross-correlation; Seismology; SIGNAL (programming language); Microseism; Passive seismic; Surface wave; Physics; Optics; Computer science; Interferometry; Mathematics; Statistics","score_opus":0.03162128833014182,"score_gpt":0.30216012223455097,"score_spread":0.27053883390440914,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1986739614","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7676975,0.00014253707,0.23027614,0.00005391909,0.0000151069125,0.000029434363,0.0003738867,0.00050372304,0.00090775173],"genre_scores_gemma":[0.8832466,0.00008068261,0.115604736,0.000021415126,0.000012932642,0.00003089654,0.0006119619,0.0000631129,0.00032759676],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998103,0.000027153235,0.000013893828,0.000047112164,0.00007854824,0.000023036895],"domain_scores_gemma":[0.99971896,0.0000900355,0.000048465383,0.000051977622,0.00007496171,0.000015501462],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035891688,0.00049059547,0.00026952487,0.0012081353,0.00018438433,0.00055610744,0.00035076865,0.0003000168,0.0004093723],"category_scores_gemma":[0.0009894393,0.00021071585,0.00037603552,0.0009439934,0.00029632472,0.00068561744,0.0005699701,0.00026251998,0.0001534118],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038559333,0.0002064215,0.06905426,0.00019162195,0.00025810068,0.00042539777,0.00034969114,0.15527524,0.5650599,0.0019307572,0.00086255505,0.20600052],"study_design_scores_gemma":[0.000039038496,0.000079438054,0.07021645,0.000013608638,0.00005528714,0.00018908785,0.000087130386,0.839066,0.08822744,0.0008876758,0.0010883029,0.000050460632],"about_ca_topic_score_codex":0.0039994023,"about_ca_topic_score_gemma":0.0051857014,"teacher_disagreement_score":0.0039994023,"about_ca_system_score_codex":0.0003228345,"about_ca_system_score_gemma":0.0004578319,"threshold_uncertainty_score":0.007952273},"labels":[],"label_agreement":null},{"id":"W2000722624","doi":"10.1002/2013jb010920","title":"Prediction of the mechanical response of hydrate‐bearing sands","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":81,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Hydrate; Permafrost; Geology; Geotechnical engineering; Submarine pipeline; Methane; Clathrate hydrate; Bearing (navigation); Constitutive equation; Thermodynamics; Chemistry; Finite element method; Oceanography","score_opus":0.034391749789243,"score_gpt":0.2973868605397635,"score_spread":0.2629951107505205,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2000722624","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97980314,0.000024084515,0.018955473,0.000013500759,0.0000027983601,0.000015019403,0.00011914237,0.000071601724,0.0009952658],"genre_scores_gemma":[0.99758554,0.000016364376,0.002139864,0.0000010867958,5.9745076e-7,0.000009085695,0.000048795962,0.0000044035805,0.00019431463],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999573,0.000008804378,0.0000028123525,0.00000906112,0.000014438537,0.0000075283133],"domain_scores_gemma":[0.999803,0.00010654158,0.000031304622,0.000014012461,0.000033692424,0.000011417339],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016952904,0.00032066583,0.0001727688,0.00037744752,0.00014690777,0.00022772825,0.00022896926,0.00037490245,0.0006349967],"category_scores_gemma":[0.00057913153,0.00015871368,0.00023558844,0.00023070988,0.00025356945,0.00017272762,0.0001447809,0.0001385908,0.00011149584],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007186605,0.000041113482,0.011751043,0.000026668125,0.000011135753,0.000059175643,0.000019520423,0.9505955,0.03215741,0.00020374294,0.000037679165,0.005025118],"study_design_scores_gemma":[0.0000037424145,0.000026327021,0.00511883,0.0000015981071,0.000002665775,0.000008930859,0.000009483965,0.9880882,0.0066407416,0.000050055864,0.00004630364,0.0000030732724],"about_ca_topic_score_codex":0.0062058633,"about_ca_topic_score_gemma":0.004877449,"teacher_disagreement_score":0.0062058633,"about_ca_system_score_codex":0.00035273324,"about_ca_system_score_gemma":0.00032555065,"threshold_uncertainty_score":0.012339473},"labels":[],"label_agreement":null},{"id":"W2006217828","doi":"10.1002/2013jb010817","title":"Modeling shear wave splitting due to stress‐induced anisotropy, with an application to Mount Asama Volcano, Japan","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"State Key Laboratory of Synthetical Automation for Process Industries; Victoria University of Wellington; University of Victoria","keywords":"Anisotropy; Volcano; Geology; Stress field; Stress (linguistics); Shear wave splitting; Shear stress; Seismology; Shear (geology); Geophysics; Mechanics; Petrology; Optics; Structural engineering; Finite element method; Engineering; Physics","score_opus":0.04384439226394852,"score_gpt":0.31229362282352646,"score_spread":0.2684492305595779,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2006217828","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9912203,0.00005315099,0.007732775,0.00007288606,0.000007709856,0.0000101524065,0.000052272695,0.000067501285,0.0007832646],"genre_scores_gemma":[0.9976629,0.000027396634,0.0021167737,0.0000042542447,0.0000034352186,0.000006216901,0.000034089455,0.000007815431,0.00013710317],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999232,0.000017334198,0.0000052661867,0.00002150286,0.000015804659,0.000016776],"domain_scores_gemma":[0.9996879,0.0001309772,0.00006003938,0.000034891516,0.000050594594,0.000035479592],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023779484,0.0005687485,0.00034787753,0.00038752006,0.00047063344,0.00066041946,0.0004688301,0.0008404267,0.00037494896],"category_scores_gemma":[0.0008371789,0.0004260216,0.00063078606,0.0004223647,0.00048617268,0.0003408707,0.00032629794,0.00032309318,0.000054897122],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003364004,0.0000404061,0.00974082,0.000009702172,0.000020546004,0.000093351926,0.000037121077,0.9814767,0.006059829,0.0003508155,0.00004933141,0.002087718],"study_design_scores_gemma":[0.000003721755,0.000006599375,0.001117682,5.267508e-7,0.0000025072995,0.000004756517,0.0000060773164,0.99856,0.00024157672,0.00003238944,0.00002193371,0.0000022930421],"about_ca_topic_score_codex":0.044159155,"about_ca_topic_score_gemma":0.020537807,"teacher_disagreement_score":0.044159155,"about_ca_system_score_codex":0.00077909173,"about_ca_system_score_gemma":0.00073192385,"threshold_uncertainty_score":0.0878042},"labels":[],"label_agreement":null},{"id":"W2015492492","doi":"10.1002/2014jb011638","title":"Multiparameter adjoint tomography of the crust and upper mantle beneath East Asia: 1. Model construction and comparisons","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":167,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Mantle (geology); Subduction; Crust; Seismology; Transition zone; Tectonics; Seismic tomography; Geophysics","score_opus":0.06514569360163264,"score_gpt":0.3020480019943682,"score_spread":0.23690230839273557,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2015492492","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9265551,0.000111503876,0.06917942,0.00022248167,0.000014138741,0.00004649033,0.0007946723,0.00043681602,0.0026393582],"genre_scores_gemma":[0.9896315,0.00004259299,0.009661006,0.000017019926,0.0000051496127,0.000044703782,0.00024133034,0.00002693828,0.00032977675],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999422,0.000018050428,0.000004843672,0.000015288551,0.000010376507,0.000009184864],"domain_scores_gemma":[0.9998276,0.00006867671,0.000029137122,0.000026072308,0.000031532007,0.000016921524],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025957788,0.00048652638,0.00032617757,0.00033481888,0.00025065689,0.0006015776,0.00089085806,0.0008376505,0.0009144617],"category_scores_gemma":[0.0007892174,0.0003512075,0.0006409489,0.0003490331,0.00046576015,0.00040588458,0.0005761481,0.0004818251,0.00011783152],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016959602,0.00001810435,0.002414671,0.000005640403,0.00001019914,0.000023707744,0.000010178095,0.9947619,0.0009212738,0.00031892842,0.00002981881,0.0014685524],"study_design_scores_gemma":[0.0000056465474,0.0000057131783,0.00043761995,7.045357e-7,0.0000023669663,0.0000038686026,0.000003341518,0.99918383,0.00017295343,0.00014788935,0.000033579046,0.00000251875],"about_ca_topic_score_codex":0.024370791,"about_ca_topic_score_gemma":0.007339338,"teacher_disagreement_score":0.024370791,"about_ca_system_score_codex":0.00058311725,"about_ca_system_score_gemma":0.0007143306,"threshold_uncertainty_score":0.04845786},"labels":[],"label_agreement":null},{"id":"W2021217603","doi":"10.1002/2014jb011426","title":"Numerical modeling of the Mount Meager landslide constrained by its force history derived from seismic data","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":96,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Resources Canada; U.S. Geological Survey; Agence Nationale de la Recherche; National Science Foundation","keywords":"Geology; Landslide; Seismology; Rockslide; Geodesy; Debris flow; Waveform; Mount; Amplitude; Debris; Geotechnical engineering; Physics; Engineering","score_opus":0.07534358011772016,"score_gpt":0.3122110916861286,"score_spread":0.23686751156840843,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2021217603","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976634,0.000022690192,0.0010640655,0.000048855647,0.0000028192962,0.000008991186,0.00013733657,0.00003593023,0.0010159184],"genre_scores_gemma":[0.99922407,0.000015587248,0.0004512929,0.0000043500568,0.0000013121816,0.0000053595218,0.00007858203,0.0000045469883,0.00021489825],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999409,0.000010416034,0.0000031767865,0.000011728094,0.000011390785,0.000022329787],"domain_scores_gemma":[0.99968064,0.0001614639,0.000060967377,0.000020787049,0.000037184225,0.00003887208],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022804351,0.00038824795,0.00027961744,0.00060553843,0.00047772887,0.00066818093,0.00063112134,0.00085906556,0.0010627785],"category_scores_gemma":[0.0012737171,0.00037492087,0.00031052702,0.00040953624,0.00067303947,0.00024578156,0.00033497406,0.0003573917,0.00007776893],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004984998,0.00003263846,0.008169512,0.000009979224,0.00001641262,0.00013335752,0.00002777259,0.98890394,0.0014845628,0.00024844208,0.00007050889,0.00085298397],"study_design_scores_gemma":[0.000007663577,0.0000100235775,0.0042184507,0.0000018796529,0.0000038440594,0.0000065216577,0.000014522346,0.9954899,0.00017075846,0.00003945686,0.000032873755,0.000004111107],"about_ca_topic_score_codex":0.23747972,"about_ca_topic_score_gemma":0.15216991,"teacher_disagreement_score":0.7625203,"about_ca_system_score_codex":0.0017020734,"about_ca_system_score_gemma":0.0010772066,"threshold_uncertainty_score":0.47219485},"labels":[],"label_agreement":null},{"id":"W2023296714","doi":"10.1002/2014jb011713","title":"Reexamination of magnetotelluric responses and electrical anisotropy of the lithospheric mantle in the Grenville Province, Canada","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Manitoba","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Lithosphere; Magnetotellurics; Anisotropy; Geophysics; Mantle (geology); Seismology; Electrical resistivity and conductivity; Front (military); Archean; Proterozoic; Geothermal gradient; Tectonics; Petrology; Paleontology; Physics","score_opus":0.038871329752919036,"score_gpt":0.301346175101238,"score_spread":0.262474845348319,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2023296714","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9953276,0.0003779103,0.00018429369,0.00009676566,0.0000043901787,0.000011443498,0.0012277632,0.000018958168,0.0027508892],"genre_scores_gemma":[0.9976305,0.00016558597,0.00038544362,0.000023987075,0.0000017235662,0.0000039768897,0.0008425526,0.0000064806036,0.0009397202],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998073,0.000010649018,0.000007500856,0.000041259274,0.000063117026,0.000070163376],"domain_scores_gemma":[0.99971277,0.000019623203,0.000025419122,0.000012864879,0.0001949161,0.00003431891],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022446281,0.00031236556,0.00026095958,0.0016373581,0.0011440989,0.00076328934,0.0005552235,0.00024507652,0.00084500783],"category_scores_gemma":[0.0005217432,0.0001822086,0.00024984017,0.0018599817,0.00039442387,0.00017540388,0.00042093618,0.000318224,0.00014731051],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002461864,0.00003510939,0.89595497,0.000107438515,0.00011433303,0.0006641501,0.0022454446,0.001991457,0.058418788,0.00045405733,0.00083405914,0.03893396],"study_design_scores_gemma":[0.0000040692235,0.000005855699,0.9964715,0.000012186309,0.000009963188,0.0000462218,0.00058778696,0.00059333694,0.00080139574,0.000018947565,0.0014425,0.000006299694],"about_ca_topic_score_codex":0.9879125,"about_ca_topic_score_gemma":0.99380565,"teacher_disagreement_score":0.012087524,"about_ca_system_score_codex":0.009504966,"about_ca_system_score_gemma":0.006727923,"threshold_uncertainty_score":0.06896365},"labels":[],"label_agreement":null},{"id":"W2059977250","doi":"10.1002/2014jb011004","title":"Thermo‐poro‐mechanics of chemically active creeping faults: 3. The role of serpentinite in episodic tremor and slip sequences, and transition to chaos","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":64,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"CMG Reservoir Simulation Foundation; National Science Foundation","keywords":"Geology; Subduction; Seismology; Trench; Slip (aerodynamics); Geophysics; Tectonics; Physics; Materials science; Nanotechnology","score_opus":0.020681724787690706,"score_gpt":0.28110977718006136,"score_spread":0.26042805239237066,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2059977250","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976889,0.00009734004,0.0011229159,0.00004825345,0.0000025226902,0.0000044293297,0.000051793875,0.000020202733,0.0009637248],"genre_scores_gemma":[0.9998179,0.000024833327,0.00006039752,0.0000015954719,0.0000013373158,7.860242e-7,0.000010534002,0.0000018315723,0.00008082837],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999695,0.0000035371238,0.0000026196333,0.000009403804,0.000007289484,0.000007638687],"domain_scores_gemma":[0.9998789,0.000019118175,0.000055730656,0.000012409684,0.000015431808,0.000018396697],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010993955,0.00021286582,0.0001706733,0.0005074283,0.00021322272,0.0005913363,0.00029079366,0.00032090498,0.0011093916],"category_scores_gemma":[0.00025985896,0.00017864157,0.00019567003,0.00017553222,0.0006114944,0.00038931094,0.00031665902,0.00016497639,0.00012107179],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00050953054,0.0001999053,0.30314288,0.0002783069,0.00011856497,0.0022264235,0.00074983726,0.2372718,0.4276044,0.012322665,0.00040707164,0.015168618],"study_design_scores_gemma":[0.000031268683,0.00013928351,0.42090136,0.000012031835,0.000028782391,0.00041474812,0.00035330444,0.55342126,0.019263886,0.004579887,0.0008121458,0.000041989668],"about_ca_topic_score_codex":0.0026052091,"about_ca_topic_score_gemma":0.0017460572,"teacher_disagreement_score":0.0026052091,"about_ca_system_score_codex":0.00035156694,"about_ca_system_score_gemma":0.00016080904,"threshold_uncertainty_score":0.005180061},"labels":[],"label_agreement":null},{"id":"W2075493090","doi":"10.1002/2013jb010452","title":"Assessment of the capabilities of the temporal and spatiotemporal ICA method for geophysical signal separation in GRACE data","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Independent component analysis; Principal component analysis; Independence (probability theory); SIGNAL (programming language); Computer science; Pattern recognition (psychology); Artificial intelligence; Statistics; Mathematics","score_opus":0.09313548335928691,"score_gpt":0.4050368372589433,"score_spread":0.3119013538996564,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2075493090","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.52047974,0.0019148901,0.46780527,0.001289573,0.00017325082,0.00016713775,0.000983582,0.0010080619,0.0061786035],"genre_scores_gemma":[0.7718665,0.00080962555,0.22447084,0.000104559775,0.00013739837,0.00017824883,0.0011836526,0.00016053297,0.0010886685],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99870336,0.0006760932,0.00007586366,0.00016445492,0.00026888202,0.000111413916],"domain_scores_gemma":[0.9883083,0.009164957,0.0005112166,0.00069787784,0.0011137994,0.00020378394],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.007214049,0.0009207092,0.00038538902,0.0014906696,0.00041455,0.0009627141,0.00043974232,0.00094648753,0.0011684423],"category_scores_gemma":[0.017714703,0.00024335604,0.0009994397,0.0012530361,0.0006092431,0.001398936,0.0009145409,0.0008341864,0.00041885357],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0030896063,0.00038245984,0.049550507,0.00041786965,0.0010172693,0.00025186938,0.00037259786,0.39588687,0.034227286,0.010018371,0.003608158,0.50117713],"study_design_scores_gemma":[0.00007552815,0.00038266878,0.025046838,0.000036167887,0.00014207074,0.00014013343,0.00011948049,0.9623272,0.008878233,0.0015698309,0.0012068328,0.00007511002],"about_ca_topic_score_codex":0.0048197303,"about_ca_topic_score_gemma":0.0057236953,"teacher_disagreement_score":0.007214049,"about_ca_system_score_codex":0.00034235447,"about_ca_system_score_gemma":0.0010699378,"threshold_uncertainty_score":0.03815204},"labels":[],"label_agreement":null},{"id":"W2083881562","doi":"10.1002/2014jb011064","title":"Influence of microscale heterogeneity and microstructure on the tensile behavior of crystalline rocks","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Rock Mechanics and Modeling","field":"Engineering","cited_by":175,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada); University of Toronto","funders":"","keywords":"Microscale chemistry; Materials science; Ultimate tensile strength; Brittleness; Microstructure; Fracture (geology); Composite material; Stress (linguistics); Computer simulation; Phase (matter); Mechanics; Mathematics","score_opus":0.02106310479010202,"score_gpt":0.2958381023521434,"score_spread":0.2747749975620414,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2083881562","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99834657,0.000048198668,0.0012419604,0.000007258973,9.239325e-7,0.000004643484,0.000036183166,0.000016262715,0.00029790736],"genre_scores_gemma":[0.99984443,0.000010904732,0.000097772194,0.0000010449368,5.3547666e-7,0.0000012885931,0.00001181157,0.000002138635,0.000030211215],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.999912,0.000009407857,0.0000054863144,0.000021365991,0.00003523315,0.000016386371],"domain_scores_gemma":[0.9996346,0.00015877547,0.000090057016,0.00004280685,0.0000428696,0.000030751682],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014126296,0.00011748014,0.00014355674,0.00023112688,0.00016735216,0.0002572354,0.000109809014,0.000121806304,0.0005688196],"category_scores_gemma":[0.00058548164,0.00015257283,0.00009325694,0.00010359754,0.00028602633,0.00016649537,0.000118748445,0.00013243717,0.000064919615],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010828778,0.00003743657,0.019408332,0.000048593898,0.000027632046,0.00027752886,0.000057090216,0.040614408,0.9350781,0.00026818615,0.000053608997,0.0040208455],"study_design_scores_gemma":[0.000023203642,0.0004542466,0.27398115,0.000012686023,0.00004056164,0.0004913572,0.00022677644,0.17035857,0.5534918,0.0003015365,0.00058989803,0.000028299042],"about_ca_topic_score_codex":0.001990154,"about_ca_topic_score_gemma":0.0036543785,"teacher_disagreement_score":0.001990154,"about_ca_system_score_codex":0.00023534936,"about_ca_system_score_gemma":0.00019611682,"threshold_uncertainty_score":0.0039570928},"labels":[],"label_agreement":null},{"id":"W2088738142","doi":"10.1002/2014jb011144","title":"Source scaling relations and along‐strike segmentation of slow slip events in a 3‐D subduction fault model","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Scaling; Slip (aerodynamics); Geology; Subduction; Seismology; Geometry; Physics; Mathematics; Tectonics","score_opus":0.038370950813599425,"score_gpt":0.3150976815281044,"score_spread":0.276726730714505,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2088738142","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97659,0.000113785325,0.018770441,0.00019245979,0.000010937219,0.000029021028,0.0007300427,0.00018895486,0.003374449],"genre_scores_gemma":[0.9981675,0.000045867222,0.0011805674,0.000010306607,0.0000034229952,0.000022086075,0.0001516684,0.000014475811,0.00040413634],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999329,0.000016391092,0.0000058336927,0.00001812516,0.000010455381,0.000016218835],"domain_scores_gemma":[0.99969316,0.00013220988,0.00007633996,0.000025558977,0.000039398692,0.00003321226],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002049467,0.0005013181,0.000481403,0.000539042,0.0003653524,0.00072323397,0.00082725973,0.001157993,0.00096295535],"category_scores_gemma":[0.00076199067,0.00035081714,0.00078258995,0.00043055235,0.0005733223,0.00035566572,0.000398196,0.00048420086,0.000112655376],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015702786,0.000014153002,0.0017443972,0.0000044172616,0.000006913184,0.000031684463,0.000012574935,0.996949,0.00044592476,0.000390814,0.00004118945,0.00034318096],"study_design_scores_gemma":[0.0000032641528,0.0000043087266,0.00041109262,8.2407223e-7,0.0000019031881,0.0000028561276,0.00000324079,0.9993888,0.00004332756,0.000114270006,0.00002390809,0.0000022028094],"about_ca_topic_score_codex":0.0470305,"about_ca_topic_score_gemma":0.012736198,"teacher_disagreement_score":0.0470305,"about_ca_system_score_codex":0.0011322184,"about_ca_system_score_gemma":0.0005988785,"threshold_uncertainty_score":0.09351355},"labels":[],"label_agreement":null},{"id":"W2095961558","doi":"10.1002/2015jb011941","title":"Recovery of secular deformation field of Mojave Shear Zone in Southern California from historical terrestrial and GPS measurements","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"National Natural Science Foundation of China; McGill University; Massachusetts Institute of Technology; National Science Foundation","keywords":"Geology; Geodesy; North American Plate; Shear zone; Seismology; Global Positioning System; Shear (geology); Secular variation; Crust; Plate tectonics; Tectonics; Geophysics; Paleontology","score_opus":0.08517724420306692,"score_gpt":0.3044581269572219,"score_spread":0.21928088275415497,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2095961558","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964095,0.00014949859,0.0003720883,0.000036870835,0.0000063995635,0.000007558362,0.0017665972,0.00008129051,0.0011702358],"genre_scores_gemma":[0.99624926,0.00011221422,0.00055881875,0.00000843478,0.0000056868244,0.000006789265,0.0024747998,0.000009398288,0.0005746009],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998896,0.000008813257,0.000006809253,0.000047842215,0.0000313022,0.000015526777],"domain_scores_gemma":[0.9996283,0.000031239448,0.0001093172,0.000058230657,0.00013025019,0.000042664502],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023541242,0.0002129247,0.00018588958,0.00090135913,0.00026489445,0.00057516625,0.00035352248,0.00023797719,0.00072247],"category_scores_gemma":[0.00075501873,0.00017273206,0.00013221169,0.00071378413,0.00014985197,0.0002086878,0.00025386384,0.00021730084,0.00019685608],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014802058,0.000056197227,0.9530789,0.000043013144,0.00009226797,0.000074297226,0.00035231057,0.008434232,0.0029539338,0.00010098576,0.0018677511,0.032798063],"study_design_scores_gemma":[0.000006855772,0.000012580674,0.9932266,0.000012086399,0.000013394919,0.000010960539,0.00007239485,0.0053711003,0.00021743748,0.000011990398,0.0010401908,0.000004525368],"about_ca_topic_score_codex":0.19965424,"about_ca_topic_score_gemma":0.3311483,"teacher_disagreement_score":0.19965424,"about_ca_system_score_codex":0.0006105542,"about_ca_system_score_gemma":0.00043643193,"threshold_uncertainty_score":0.39698422},"labels":[],"label_agreement":null},{"id":"W2096615428","doi":"10.1002/2015jb012270","title":"Limitations on silicon in the outer core: Ultrasonic measurements at high temperatures and high d<i>K</i>/d<i>P</i> values of Fe‐Ni‐Si liquids at high pressures","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; University of Hawai'i; National Science Foundation","keywords":"Materials science; Bulk modulus; Silicon; Isothermal process; Elastic modulus; Ultrasonic sensor; Analytical Chemistry (journal); Elasticity (physics); High pressure; Thermodynamics; Composite material; Metallurgy; Chemistry; Organic chemistry","score_opus":0.12297395898668054,"score_gpt":0.3227110052730766,"score_spread":0.19973704628639607,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2096615428","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98207766,0.00051537284,0.012307015,0.00010016936,0.000012994855,0.000012613233,0.00024643505,0.00016019511,0.004567509],"genre_scores_gemma":[0.99810565,0.0001257958,0.0013183872,0.000017746897,0.000005129305,0.0000069809053,0.00011563549,0.000020372527,0.000284429],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9996444,0.000028823157,0.000016262069,0.00006500468,0.00019220852,0.00005333327],"domain_scores_gemma":[0.9995541,0.00019251404,0.00005998991,0.000041759416,0.00012235303,0.000029242434],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038114857,0.0003042273,0.0003089822,0.00046073174,0.00032562733,0.00058684027,0.00053634157,0.00041793167,0.0015122944],"category_scores_gemma":[0.0010211811,0.00026947763,0.00014551762,0.00042825317,0.0010917089,0.0009374826,0.0007565085,0.00046661828,0.00043056675],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012169166,0.0000137591205,0.0052043805,0.00007483404,0.000005344327,0.00010486136,0.00020900543,0.00049289217,0.98731995,0.0004623423,0.00006079986,0.0059301537],"study_design_scores_gemma":[0.0000059882327,0.00008753584,0.014609774,0.0000122869615,0.0000087988665,0.00014835352,0.00016385585,0.0031115825,0.9806982,0.00020591012,0.00093525014,0.000012588071],"about_ca_topic_score_codex":0.0018480143,"about_ca_topic_score_gemma":0.0019557152,"teacher_disagreement_score":0.0018480143,"about_ca_system_score_codex":0.00027861368,"about_ca_system_score_gemma":0.00032128335,"threshold_uncertainty_score":0.005059123},"labels":[],"label_agreement":null},{"id":"W2097974352","doi":"10.1002/jgrb.50255","title":"Magnetotelluric constraints on the fluid content in the upper mantle beneath the southern Canadian Cordillera: Implications for rheology","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Asthenosphere; Mantle wedge; Mantle (geology); Subduction; Lithosphere; Craton; Crust; Petrology; Geophysics; Transition zone; Seismology; Tectonics","score_opus":0.0854821186198172,"score_gpt":0.3215658926951853,"score_spread":0.23608377407536812,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2097974352","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9965018,0.00043326218,0.0002194139,0.00012226241,0.0000026783553,0.0000069815487,0.0006105241,0.00003203358,0.0020710411],"genre_scores_gemma":[0.9989741,0.00016690015,0.00028120133,0.0000123218715,0.0000015925982,0.0000035059072,0.00030652498,0.000004174409,0.0002498339],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999884,0.000004478566,0.000005047099,0.000032024593,0.00003132239,0.000043110816],"domain_scores_gemma":[0.9998104,0.000020361016,0.000028116754,0.000008824871,0.00010074269,0.00003155604],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016889206,0.00060377014,0.0002967482,0.0018569654,0.001684666,0.0010684198,0.00062065624,0.0003311785,0.0012606112],"category_scores_gemma":[0.0008378105,0.00020277128,0.00026036386,0.0019358662,0.00050891365,0.0003433072,0.00046575707,0.00022223195,0.00012332153],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030709844,0.000041340594,0.8786009,0.00016043895,0.00013593091,0.00040684204,0.001318419,0.009411504,0.07661213,0.0014076506,0.00052349846,0.031074274],"study_design_scores_gemma":[0.0000074375,0.0000110593755,0.9922099,0.000017596078,0.000023921968,0.000036536912,0.00043961886,0.004109294,0.0019085322,0.0001229713,0.0010952543,0.000017767094],"about_ca_topic_score_codex":0.9556695,"about_ca_topic_score_gemma":0.969316,"teacher_disagreement_score":0.044330478,"about_ca_system_score_codex":0.010639754,"about_ca_system_score_gemma":0.004677718,"threshold_uncertainty_score":0.08918303},"labels":[],"label_agreement":null},{"id":"W2098899733","doi":"10.1002/2014jb011353","title":"Crustal imprints of Precambrian orogenesis in western Laurentia","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Precambrian; Geology; Craton; Baltica; Laurentia; Crust; Rodinia; Terrane; Geochemistry; Shear zone; Basement; Subduction; Paleontology; Petrology; Tectonics; Ordovician","score_opus":0.06647104350929389,"score_gpt":0.3253319640687748,"score_spread":0.2588609205594809,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2098899733","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963637,0.00023902796,0.000026674637,0.0000304311,0.0000014674786,0.0000026779994,0.00020970165,0.000007935914,0.0031184263],"genre_scores_gemma":[0.9993362,0.00008889135,0.00004558873,0.000005928178,0.0000011938263,0.0000011055903,0.00011775999,0.0000024012932,0.00040100585],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990463,0.000007234102,0.0000047451813,0.000025124353,0.000018147166,0.000040068466],"domain_scores_gemma":[0.99975353,0.000018057028,0.00009751394,0.0000132162595,0.00006770659,0.000049971106],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000106650135,0.00017837588,0.00013797515,0.0014678471,0.00042857107,0.0007662884,0.00024105827,0.00008955098,0.0014665653],"category_scores_gemma":[0.00043636994,0.00009442551,0.00011078863,0.00091919105,0.0003242519,0.00017390525,0.0004727634,0.00009434127,0.00019085156],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016011405,0.000014414333,0.9468333,0.00007178432,0.000081480415,0.0009434265,0.0034374127,0.00060376414,0.023772689,0.00044340477,0.00031513133,0.023323083],"study_design_scores_gemma":[7.326618e-7,0.0000027472552,0.9991093,0.000008615894,0.0000035398427,0.000031367537,0.00025241004,0.00008141335,0.00013366624,0.000011358899,0.00036293926,0.0000019215513],"about_ca_topic_score_codex":0.5345329,"about_ca_topic_score_gemma":0.81575114,"teacher_disagreement_score":0.5345329,"about_ca_system_score_codex":0.0022284724,"about_ca_system_score_gemma":0.0011218409,"threshold_uncertainty_score":0.9364166},"labels":[],"label_agreement":null},{"id":"W2102311688","doi":"10.1002/2013jb010730","title":"Variations in axial magma lens properties along the East Pacific Rise (9°30′N–10°00′N) from swath 3‐D seismic imaging and 1‐D waveform inversion","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Science Foundation","keywords":"Geology; Magma chamber; Seismology; Magma; Waveform; Mineralogy; Petrology; Volcano; Physics","score_opus":0.028574294475197614,"score_gpt":0.2406308177294683,"score_spread":0.21205652325427068,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2102311688","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974111,0.000024823257,0.0007880364,0.000019584335,0.0000022507309,0.000005310702,0.00041433872,0.00007938512,0.0012552175],"genre_scores_gemma":[0.99766624,0.000036515925,0.0012385772,0.000006385315,0.0000024697863,0.0000039524853,0.0008117658,0.000018522074,0.00021548683],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992824,0.0000047362328,0.0000036835054,0.000019694182,0.000029436771,0.000014236307],"domain_scores_gemma":[0.9998361,0.000025838266,0.00003529709,0.0000117947675,0.000066087516,0.000024916308],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013119845,0.00023846349,0.00014959343,0.0006690995,0.00021103109,0.00058916165,0.00018811678,0.00019028899,0.0007712509],"category_scores_gemma":[0.00043072377,0.00026817253,0.00024243661,0.00070352043,0.0001946763,0.00026796473,0.00025943364,0.00024631785,0.00014547214],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036046913,0.00012152121,0.7429125,0.0000827983,0.00019817533,0.0005748887,0.0007530002,0.029815339,0.1640688,0.0003788226,0.0012406943,0.059493057],"study_design_scores_gemma":[0.000009863702,0.000013107284,0.9662979,0.000005452217,0.000024139457,0.00008097639,0.00013581806,0.026469547,0.006333432,0.000033911958,0.00058276654,0.000013065027],"about_ca_topic_score_codex":0.04930322,"about_ca_topic_score_gemma":0.09899732,"teacher_disagreement_score":0.04930322,"about_ca_system_score_codex":0.0004033783,"about_ca_system_score_gemma":0.00048782874,"threshold_uncertainty_score":0.098032534},"labels":[],"label_agreement":null},{"id":"W2102412510","doi":"10.1002/2013jb010836","title":"An investigation of seismicity clustered near the Cordel Field, west central Alberta, and its relation to a nearby disposal well","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":108,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"University of Alberta","keywords":"Induced seismicity; Seismology; Hypocenter; Geology; Foreland basin; Structural basin; Tectonics; Paleontology","score_opus":0.02634559759588099,"score_gpt":0.29178186278990065,"score_spread":0.26543626519401964,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2102412510","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984263,0.000055792003,0.00014117552,0.000019604642,0.0000020497296,0.000011097634,0.0003310127,0.000010160788,0.0010029029],"genre_scores_gemma":[0.9981579,0.00007671577,0.0003149675,0.000008920712,0.0000028263703,0.0000055951937,0.0005273403,0.000002215181,0.0009034906],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985003,0.000006981324,0.0000052084747,0.000031766904,0.00006730341,0.000038586335],"domain_scores_gemma":[0.9995622,0.000041972886,0.00008858677,0.000016634633,0.00018313921,0.000107506756],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012979831,0.00023907884,0.00017647032,0.0017609348,0.00086061604,0.0005997176,0.0004986364,0.00022639768,0.0007924802],"category_scores_gemma":[0.0005002066,0.00011592995,0.00009013485,0.0022587692,0.0004338308,0.0001293424,0.00042886066,0.0002104506,0.000085443724],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016391824,0.00007011757,0.9631197,0.00003192633,0.000033693956,0.0006523772,0.0016105538,0.0009295759,0.01198944,0.00014561211,0.0004964516,0.020756572],"study_design_scores_gemma":[0.0000024431895,0.00002110666,0.9972675,0.000004664272,0.0000072311136,0.000039234114,0.0011511473,0.0006369446,0.00036267997,0.000010068517,0.0004927903,0.000004308542],"about_ca_topic_score_codex":0.8734016,"about_ca_topic_score_gemma":0.9632982,"teacher_disagreement_score":0.12659842,"about_ca_system_score_codex":0.0036454496,"about_ca_system_score_gemma":0.0036864514,"threshold_uncertainty_score":0.2546879},"labels":[],"label_agreement":null},{"id":"W2102626288","doi":"10.1002/jgrb.50390","title":"Downdip landward limit of Cascadia great earthquake rupture","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":98,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Seismology; Subduction; Seismic hazard; Slip (aerodynamics); Episodic tremor and slip; Thrust; Submarine pipeline; Thrust fault; Earthquake rupture; Tectonics; Geotechnical engineering; Fault (geology)","score_opus":0.04129512463622898,"score_gpt":0.3013903984514716,"score_spread":0.2600952738152426,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2102626288","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9724654,0.0005499778,0.0010489773,0.00021859966,0.000010775789,0.000012180747,0.00074692734,0.000071362214,0.024875863],"genre_scores_gemma":[0.9987865,0.00009744313,0.000101855556,0.00002225862,0.000008060185,0.0000056937656,0.00041424687,0.000006834838,0.0005569471],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996687,0.00005686544,0.00003075168,0.00006218252,0.000115851595,0.000065638305],"domain_scores_gemma":[0.99796236,0.00048204666,0.0005089638,0.00018589968,0.000602631,0.00025808756],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005137694,0.00021129103,0.00024466723,0.0011981786,0.0004945891,0.0009881802,0.00035452744,0.0002500816,0.0054071],"category_scores_gemma":[0.0038741434,0.0001252847,0.00016455079,0.00042730485,0.00047796685,0.00046650285,0.0009525506,0.0002408304,0.0007495879],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003923343,0.000029324,0.9452806,0.00017053858,0.00007318157,0.00085221895,0.0010073811,0.009734099,0.015529708,0.0025232083,0.00199102,0.022416363],"study_design_scores_gemma":[0.000008396414,0.00006630368,0.98898447,0.000053065807,0.000016939062,0.00027105445,0.0007541558,0.002831479,0.0015551918,0.0009572122,0.004486008,0.000015669626],"about_ca_topic_score_codex":0.015070873,"about_ca_topic_score_gemma":0.019918764,"teacher_disagreement_score":0.015070873,"about_ca_system_score_codex":0.00055750506,"about_ca_system_score_gemma":0.00034230243,"threshold_uncertainty_score":0.029966354},"labels":[],"label_agreement":null},{"id":"W2109185446","doi":"10.1002/2015jb012200","title":"Steadily propagating slip pulses driven by thermal decomposition","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Science Foundation","keywords":"Cabin pressurization; Thermal decomposition; Slip (aerodynamics); Thermal; Pore water pressure; Mechanics; Materials science; Decomposition; Thermodynamics; Geotechnical engineering; Geology; Composite material; Chemistry; Physics","score_opus":0.0633204400114171,"score_gpt":0.3476548493656741,"score_spread":0.284334409354257,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2109185446","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9861914,0.000099445504,0.011652021,0.000058086316,0.000014893208,0.000010175035,0.000045697903,0.00012737662,0.0018008148],"genre_scores_gemma":[0.9991091,0.00002741987,0.0005373109,0.000008311218,0.0000049068376,0.0000037133432,0.000017309896,0.0000065345093,0.00028537904],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999566,0.000004691305,0.0000029802177,0.000009769931,0.00001140527,0.000014468742],"domain_scores_gemma":[0.9998198,0.000043246575,0.00005916057,0.000018933773,0.000025091667,0.00003378482],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000115658215,0.00025500084,0.00020630284,0.00028343982,0.00013792068,0.000366675,0.00024196069,0.00033328068,0.0013142519],"category_scores_gemma":[0.00062730134,0.00017879186,0.0001690356,0.00014269802,0.0003239216,0.0002808877,0.0003016827,0.0003369978,0.000113331604],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009269226,0.0002974422,0.030836323,0.00023706698,0.00016159027,0.0026052601,0.0005648629,0.33907014,0.55654573,0.020825569,0.0013235719,0.046605486],"study_design_scores_gemma":[0.000028083496,0.00017059977,0.018513681,0.000015441807,0.000025155452,0.00021229297,0.00011034399,0.9429128,0.03426168,0.0031755378,0.0005514407,0.000022834376],"about_ca_topic_score_codex":0.0005307371,"about_ca_topic_score_gemma":0.0003749752,"teacher_disagreement_score":0.0013142519,"about_ca_system_score_codex":0.00027715706,"about_ca_system_score_gemma":0.00013389412,"threshold_uncertainty_score":0.0043966174},"labels":[],"label_agreement":null},{"id":"W2112665602","doi":"10.1002/2014jb011321","title":"Crustal anisotropy in a subduction zone forearc: Northern Cascadia","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Geology; Anisotropy; Terrane; Subduction; Seismology; Schist; Seismometer; Tectonics; Paleontology; Metamorphic rock","score_opus":0.024728495141485674,"score_gpt":0.2976169257470217,"score_spread":0.272888430605536,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2112665602","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999076,0.000011216848,0.000066802895,0.000021439775,9.116342e-7,0.000002903025,0.0001673273,0.000025939014,0.0006273645],"genre_scores_gemma":[0.99949074,0.000016470824,0.000079593825,0.0000027191597,6.4204454e-7,0.0000025744805,0.00021544384,0.000005388236,0.00018649982],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999062,0.000011668292,0.0000074930463,0.000032417305,0.000021549586,0.000020668456],"domain_scores_gemma":[0.9997154,0.000044531684,0.00004416538,0.00003396614,0.000078500125,0.00008338956],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020931155,0.0004976782,0.00031127097,0.0010412565,0.0007749596,0.0008457284,0.0005506717,0.00047251603,0.0020199134],"category_scores_gemma":[0.0007039275,0.00043543297,0.00049393706,0.0009575781,0.0004371875,0.00019334495,0.00046919874,0.00029913028,0.0002489252],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024513816,0.00009350107,0.8874618,0.000045618828,0.00023245453,0.00066263025,0.00091110414,0.08920135,0.0135824755,0.00038063995,0.0005619164,0.006621467],"study_design_scores_gemma":[0.000026894215,0.00003312231,0.95644456,0.0000085813845,0.00004605397,0.000046194775,0.0004927666,0.04189722,0.00048778314,0.00011070195,0.00038760112,0.00001842931],"about_ca_topic_score_codex":0.409,"about_ca_topic_score_gemma":0.438405,"teacher_disagreement_score":0.59099996,"about_ca_system_score_codex":0.0021658866,"about_ca_system_score_gemma":0.0011598887,"threshold_uncertainty_score":0.81323874},"labels":[],"label_agreement":null},{"id":"W2113716101","doi":"10.1002/2013jb010885","title":"Anomalous surface heave induced by enhanced oil recovery in northern Alberta: InSAR observations and numerical modeling","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysical Methods and Applications","field":"Engineering","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"Natural Resources Canada; Canadian Space Agency","keywords":"Steam injection; Wellhead; Geology; Injector; Oil sands; Interferometric synthetic aperture radar; Petroleum engineering; Asphalt; Geotechnical engineering; Petrology; Hydrology (agriculture); Synthetic aperture radar","score_opus":0.04597185728305152,"score_gpt":0.3208872141597943,"score_spread":0.2749153568767428,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2113716101","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99790275,0.00003006253,0.0004328664,0.000061296334,0.0000032283142,0.0000064741675,0.0003626901,0.00009039024,0.0011102662],"genre_scores_gemma":[0.9989761,0.000034246394,0.0003874741,0.000007873283,0.0000020020896,0.0000032095127,0.0002734414,0.0000070562464,0.00030856195],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992454,0.0000070934298,0.0000024671044,0.00001598636,0.000020932666,0.000028897686],"domain_scores_gemma":[0.9998915,0.000023741053,0.000018351246,0.000011119115,0.000027184931,0.000028108441],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021086255,0.0004476765,0.00021227442,0.00050593016,0.00066926057,0.0006528308,0.00082615216,0.00046493555,0.0008518659],"category_scores_gemma":[0.0004376808,0.0003245432,0.00032578135,0.000774548,0.00067293685,0.00022698144,0.000280145,0.0003055586,0.00012998619],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040826763,0.00029970735,0.2374152,0.000049728424,0.00010699289,0.0005042319,0.00026434442,0.7343655,0.013376321,0.00093603635,0.0012957209,0.010977905],"study_design_scores_gemma":[0.000061771505,0.000026670661,0.1446501,0.0000053082617,0.000022765465,0.00002329369,0.00019479234,0.8531993,0.0011104604,0.00018509472,0.0004879685,0.000032408505],"about_ca_topic_score_codex":0.85005355,"about_ca_topic_score_gemma":0.7958491,"teacher_disagreement_score":0.14994645,"about_ca_system_score_codex":0.004580347,"about_ca_system_score_gemma":0.002561442,"threshold_uncertainty_score":0.301659},"labels":[],"label_agreement":null},{"id":"W2116267660","doi":"10.1002/jgrb.50294","title":"Sea level variations during snowball Earth formation and evolution: 2. The influence of Earth's rotation","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; University of Toronto; Compute Canada","keywords":"Mantle (geology); Earth's rotation; Lithosphere; Snowball Earth; Geology; Convection; Geophysics; Mantle convection; Sea level; Geodesy; Mechanics; Physics; Oceanography; Tectonics; Paleontology; Glacial period","score_opus":0.029629635731009366,"score_gpt":0.28163811794983656,"score_spread":0.2520084822188272,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2116267660","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988839,0.000042663443,0.0001587964,0.000008611633,0.0000013358651,0.0000022036647,0.00030512805,0.000012544596,0.0005848627],"genre_scores_gemma":[0.9992555,0.0000264303,0.000074628515,0.000002798984,0.000001555322,0.0000018502309,0.0004632126,0.0000061074597,0.00016798543],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99994445,0.0000089544155,0.0000037636253,0.000013913939,0.000009228462,0.000019724877],"domain_scores_gemma":[0.99983656,0.00005559453,0.000040743667,0.000015624402,0.00002011988,0.00003127953],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019362888,0.0002539033,0.00024847066,0.0005324353,0.0002192852,0.00060235156,0.00019253146,0.0002737107,0.0012209394],"category_scores_gemma":[0.00043914455,0.00011004077,0.00041282485,0.00039120903,0.00018140356,0.00026611076,0.00035828393,0.00017708927,0.00026764532],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009207962,0.00006584573,0.87656575,0.000075665484,0.00017031068,0.00057967403,0.00027490905,0.018803677,0.0842866,0.0004978606,0.00029669446,0.017462272],"study_design_scores_gemma":[0.000008968474,0.00009228132,0.98385704,0.0000025625927,0.000036307258,0.00007294966,0.000086098626,0.009536587,0.005727712,0.00007427497,0.0004963913,0.000008907494],"about_ca_topic_score_codex":0.006275999,"about_ca_topic_score_gemma":0.0051701902,"teacher_disagreement_score":0.006275999,"about_ca_system_score_codex":0.00029304996,"about_ca_system_score_gemma":0.00013179166,"threshold_uncertainty_score":0.012478948},"labels":[],"label_agreement":null},{"id":"W2119243980","doi":"10.1002/2015jb012064","title":"The impacts of mantle phase transitions and the iron spin crossover in ferropericlase on convective mixing—is the evidence for compositional convection definitive? New results from a Yin‐Yang overset grid‐based control volume model","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Mantle convection; Mantle (geology); Subduction; Convection; Geophysics; Spin transition; Spin crossover; Geodynamics; Condensed matter physics; Petrology; Tectonics; Mechanics; Physics; Seismology","score_opus":0.09986677130596558,"score_gpt":0.3730705947074852,"score_spread":0.2732038234015196,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2119243980","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97435445,0.00017249878,0.020035924,0.00030629532,0.00002538061,0.000030322979,0.00025358895,0.00023636143,0.0045850966],"genre_scores_gemma":[0.99526703,0.00006607832,0.003754841,0.000028981709,0.000007835094,0.000028065882,0.000122408,0.000049583774,0.0006752654],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999006,0.000038807353,0.000004065062,0.000017014743,0.000018672716,0.000020850177],"domain_scores_gemma":[0.9993018,0.00045125806,0.00008007002,0.000040785737,0.0000603424,0.00006570276],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042615624,0.0005411356,0.0006422318,0.00035466318,0.00050323724,0.001040208,0.0011170023,0.00074065593,0.0013989687],"category_scores_gemma":[0.0015098915,0.0002768924,0.0006120233,0.00024780328,0.001018712,0.00066502317,0.00059291336,0.00059732964,0.00009563545],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000370123,0.00001844794,0.0011469141,0.000008965394,0.000011556542,0.000028594042,0.000011295598,0.9961875,0.0005795308,0.0013408816,0.00006824492,0.00056099944],"study_design_scores_gemma":[0.000011836456,0.0000074356585,0.000119510114,6.5263816e-7,0.0000022257886,0.0000019145584,0.0000028736158,0.999424,0.00010844474,0.00028733475,0.000032349337,0.0000015077065],"about_ca_topic_score_codex":0.037258074,"about_ca_topic_score_gemma":0.012484936,"teacher_disagreement_score":0.037258074,"about_ca_system_score_codex":0.0008404432,"about_ca_system_score_gemma":0.0010468449,"threshold_uncertainty_score":0.074082434},"labels":[],"label_agreement":null},{"id":"W2132896650","doi":"10.1002/jgrb.50240","title":"A double seismic zone in the subducting Juan Fernandez Ridge of the Nazca Plate (32°S), central Chile","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Slab; Seismology; Slab window; Lithosphere; Induced seismicity; Subduction; Ridge; Focal mechanism; Crust; Oceanic crust; Stress field; Mantle wedge; Volcanism; Tectonics; Geophysics; Paleontology","score_opus":0.047288889167636156,"score_gpt":0.3002259037364177,"score_spread":0.2529370145687816,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2132896650","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99737704,0.0001495509,0.000100283054,0.00002904545,0.0000029275782,0.000011031404,0.00040916554,0.00001542882,0.0019054778],"genre_scores_gemma":[0.99886864,0.00006261886,0.00013529958,0.0000048946467,0.0000024328247,0.000012011934,0.000337658,0.0000020379807,0.0005743781],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999275,0.000004245577,0.0000049539253,0.00002189363,0.000014527455,0.000026747208],"domain_scores_gemma":[0.9998524,0.00001188128,0.00005343836,0.0000113043,0.00003596095,0.000034965444],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009879607,0.00023628108,0.00017386895,0.0013920082,0.00036731214,0.0005957834,0.00030424062,0.00021715874,0.0013018015],"category_scores_gemma":[0.00034702723,0.00016542042,0.0001254315,0.0010385816,0.0004067452,0.0002046536,0.0008956732,0.00014720742,0.0001723729],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034471357,0.000076372984,0.9266656,0.00017503537,0.000090058566,0.0014697578,0.002934614,0.0011445584,0.041551888,0.0005173414,0.00061731465,0.024412747],"study_design_scores_gemma":[0.000009671489,0.000016730592,0.9970626,0.0000143638,0.000007794417,0.00010173407,0.0010412494,0.00026683992,0.00038532307,0.000042758893,0.0010460641,0.000004810059],"about_ca_topic_score_codex":0.068625264,"about_ca_topic_score_gemma":0.07597287,"teacher_disagreement_score":0.068625264,"about_ca_system_score_codex":0.00074196147,"about_ca_system_score_gemma":0.0007364763,"threshold_uncertainty_score":0.13645166},"labels":[],"label_agreement":null},{"id":"W2133222974","doi":"10.1002/2014jb011067","title":"Bayesian inference for ultralow velocity zones in the Earth's lowermost mantle: Complex ULVZ beneath the east of the Philippines","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Australian Government","keywords":"Geology; Bayesian inference; Bayesian probability; Mantle (geology); Parallel tempering; Inversion (geology); Nonlinear system; Geophysics; Algorithm; Geodesy; Seismology; Computer science; Markov chain Monte Carlo; Physics; Artificial intelligence; Tectonics","score_opus":0.05248532653138223,"score_gpt":0.3222693776096103,"score_spread":0.26978405107822806,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2133222974","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9438681,0.00013222915,0.054613516,0.00027093705,0.000004800241,0.00001855979,0.0002619019,0.00019602604,0.00063392986],"genre_scores_gemma":[0.99334854,0.000040883697,0.006251744,0.0000124737235,0.0000048935135,0.0000054726406,0.00017215322,0.000020211488,0.00014372861],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997434,0.000085434636,0.000014407721,0.00008130855,0.000045686407,0.00002981008],"domain_scores_gemma":[0.99915195,0.00042844756,0.00017376362,0.00005093453,0.00013243202,0.00006247966],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012926451,0.0003835005,0.000349087,0.0013346011,0.00039701114,0.00092821545,0.0008751329,0.00060823647,0.000763917],"category_scores_gemma":[0.004568379,0.00046202497,0.00044137746,0.00073894137,0.0005479371,0.000656396,0.0009765071,0.0005304837,0.00008450226],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001242219,0.00007189213,0.14887911,0.00006659203,0.00018773323,0.00033253906,0.0004965333,0.80412024,0.0074243844,0.0068581835,0.0005056418,0.03093293],"study_design_scores_gemma":[0.0000133788335,0.000007192239,0.037983537,0.000009620545,0.000014994805,0.0000142708295,0.00009978662,0.95844066,0.00072112813,0.002463899,0.00021271678,0.000018879147],"about_ca_topic_score_codex":0.045687634,"about_ca_topic_score_gemma":0.0380003,"teacher_disagreement_score":0.045687634,"about_ca_system_score_codex":0.0008974767,"about_ca_system_score_gemma":0.0007996945,"threshold_uncertainty_score":0.09084344},"labels":[],"label_agreement":null},{"id":"W2134909076","doi":"10.1002/2014jb011237","title":"Average<i>Q</i><sub>Lg</sub>,<i>Q</i><sub>Sn</sub>, and observation of Lg blockage in the Continental Margin of Nova Scotia","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey","keywords":"Attenuation; Amplitude; Nova scotia; Continental margin; Geology; Spectral line; Physics; Phase (matter); Geodesy; Seismology; Tectonics; Optics","score_opus":0.03513808118598524,"score_gpt":0.2813312903703435,"score_spread":0.24619320918435825,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2134909076","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99806696,0.000029834258,0.000120446224,0.000011392699,9.117441e-7,0.0000028218735,0.00041777574,0.000009481745,0.0013403299],"genre_scores_gemma":[0.9994429,0.000018833189,0.00007925742,0.0000035324742,9.312587e-7,0.000001181706,0.00023485011,0.0000023006667,0.00021619441],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999941,0.000003614167,0.000003850873,0.00001154812,0.00002219533,0.000017910075],"domain_scores_gemma":[0.99966085,0.000035638695,0.00006463842,0.000021056108,0.00016158211,0.000056288805],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012424965,0.000117166106,0.000081372615,0.00063081284,0.00038621892,0.0003363066,0.00017660751,0.000088744324,0.0007064342],"category_scores_gemma":[0.00039931684,0.00008387126,0.00008394031,0.0005496643,0.00026339674,0.00009689784,0.00020877716,0.00011070911,0.00013087608],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010488491,0.000010781262,0.97847545,0.000014984425,0.000025245918,0.00011435367,0.00019935572,0.0007328301,0.013965057,0.000060824244,0.00027452435,0.006021627],"study_design_scores_gemma":[0.0000011446916,0.0000033909234,0.99914956,0.000001375305,0.000003088213,0.000014051838,0.000066533205,0.00031062873,0.00033576196,0.0000049234714,0.0001086234,8.119022e-7],"about_ca_topic_score_codex":0.6681258,"about_ca_topic_score_gemma":0.78448653,"teacher_disagreement_score":0.3318742,"about_ca_system_score_codex":0.001317688,"about_ca_system_score_gemma":0.0006944325,"threshold_uncertainty_score":0.6676573},"labels":[],"label_agreement":null},{"id":"W2137748830","doi":"10.1002/2014jb011821","title":"Layered crustal anisotropy around the San Andreas Fault near Parkfield, California","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":94,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Crust; Anisotropy; Seismology; Seismic anisotropy; Brittleness; Deformation (meteorology); Fault (geology); Geophysics; Petrology; Mantle (geology); Materials science","score_opus":0.07337791509720246,"score_gpt":0.33172335846915146,"score_spread":0.258345443371949,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2137748830","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99868566,0.00005236464,0.00006428074,0.000033765005,0.0000013090379,0.0000025945587,0.00013532898,0.000020087044,0.0010045458],"genre_scores_gemma":[0.9995609,0.000031766744,0.00008933877,0.000003675809,0.000002182856,7.965203e-7,0.00009763816,0.000001380478,0.00021231084],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999132,0.000005680208,0.0000044998806,0.000030153966,0.000027955388,0.000018452889],"domain_scores_gemma":[0.99983644,0.000019827394,0.000048298825,0.000012036088,0.00005755117,0.000025869393],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012790972,0.0001677762,0.00015510523,0.0008561013,0.00038343013,0.00039583017,0.0002324223,0.00016677343,0.001371842],"category_scores_gemma":[0.0004207755,0.00018310083,0.000070111855,0.00041816616,0.00024068763,0.00023001124,0.00030333266,0.00015742531,0.00014846004],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021407103,0.00009668991,0.9275508,0.000052219075,0.00010139541,0.00043590143,0.00095203175,0.0047648028,0.047125757,0.00036676574,0.0007072815,0.017632237],"study_design_scores_gemma":[0.000008425488,0.000010900044,0.99688333,0.0000052277937,0.000011327963,0.000037480393,0.00018303934,0.0020091536,0.00048227364,0.000026763406,0.000337633,0.000004457552],"about_ca_topic_score_codex":0.12690319,"about_ca_topic_score_gemma":0.17900752,"teacher_disagreement_score":0.12690319,"about_ca_system_score_codex":0.00063623337,"about_ca_system_score_gemma":0.00040455072,"threshold_uncertainty_score":0.25232905},"labels":[],"label_agreement":null},{"id":"W2139034619","doi":"10.1002/jgrb.50289","title":"Magma storage and migration associated with the 2011–2012 El Hierro eruption: Implications for crustal magmatic systems at oceanic island volcanoes","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":105,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada; Western University","funders":"","keywords":"Geology; Volcano; Magma; Seismology; Underplating; Magma chamber; Subduction; Tectonics","score_opus":0.03278165837653291,"score_gpt":0.2933098242273749,"score_spread":0.260528165850842,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2139034619","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99899954,0.00008380963,0.00037461246,0.000048085065,0.0000017856587,0.0000038307357,0.00011719273,0.0000139217655,0.00035714623],"genre_scores_gemma":[0.9994935,0.000044220895,0.00025437347,0.0000046144355,0.0000026921593,0.0000015931618,0.00013117648,0.0000042898655,0.00006353008],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999461,0.000007749073,0.0000038044095,0.000020518602,0.0000064208143,0.00001533894],"domain_scores_gemma":[0.9999007,0.00002137227,0.00002973098,0.000011073839,0.000014108786,0.000023114048],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020954717,0.00036143395,0.00028578946,0.0006061528,0.0003178077,0.0008257362,0.00037875993,0.0005293304,0.00078057457],"category_scores_gemma":[0.00046616455,0.00024719918,0.0004972474,0.00046791593,0.00038541327,0.00053680467,0.0004261191,0.00027849895,0.00009008226],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019077807,0.00019120795,0.8005488,0.00008317517,0.00022699403,0.0004783459,0.0006205355,0.14390633,0.03701641,0.0012617522,0.00033616912,0.015139541],"study_design_scores_gemma":[0.000016645097,0.000044280845,0.72483635,0.000011428254,0.000038942257,0.00008887343,0.00039657755,0.2726088,0.0011119435,0.00046802804,0.00035405782,0.000024035047],"about_ca_topic_score_codex":0.041422248,"about_ca_topic_score_gemma":0.04098941,"teacher_disagreement_score":0.041422248,"about_ca_system_score_codex":0.00076268153,"about_ca_system_score_gemma":0.0004950351,"threshold_uncertainty_score":0.082362294},"labels":[],"label_agreement":null},{"id":"W2139141422","doi":"10.1002/2014jb011606","title":"The role of lithological layering and pore pressure on fluid‐induced microseismicity","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Microseismic Industry Consortium","keywords":"Microseism; Layering; Geology; Hydraulic fracturing; Shear (geology); Fluid pressure; Ultimate tensile strength; Stress field; Fracture (geology); Geotechnical engineering; Pore water pressure; Tension (geology); Shear stress; Petrology; Seismology; Mechanics; Materials science; Structural engineering; Composite material; Engineering","score_opus":0.05628980197617452,"score_gpt":0.32281828985999583,"score_spread":0.26652848788382133,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2139141422","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99820757,0.000040777846,0.001297934,0.00002216774,0.0000019548274,0.0000042319857,0.000044502147,0.000034000343,0.00034695087],"genre_scores_gemma":[0.9998678,0.0000098116125,0.00007704488,0.0000014053553,3.8161082e-7,0.000001276877,0.000008258857,0.0000021933815,0.000031777407],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99989057,0.000019463336,0.000008061033,0.000023003948,0.000017196002,0.00004168704],"domain_scores_gemma":[0.99941885,0.00030370418,0.00013917686,0.000038363167,0.00005370071,0.000046220383],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026938692,0.00031434596,0.00029961436,0.00043698354,0.00029807095,0.0005376234,0.00034283134,0.00041101055,0.0010754049],"category_scores_gemma":[0.0010061009,0.00025115995,0.00027606604,0.0002433725,0.0004765329,0.0004354977,0.00032037494,0.0002860405,0.00009831761],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031836005,0.0002378903,0.12220966,0.00007002605,0.00008063531,0.00039930403,0.000080177604,0.7333799,0.13184269,0.00074759265,0.00013640101,0.010497349],"study_design_scores_gemma":[0.00002266384,0.0001572041,0.092892796,0.0000077312625,0.0000247079,0.00004525479,0.00007513121,0.8756481,0.030693984,0.00028945904,0.00011586208,0.000027077715],"about_ca_topic_score_codex":0.006082294,"about_ca_topic_score_gemma":0.0030853227,"teacher_disagreement_score":0.006082294,"about_ca_system_score_codex":0.0006029239,"about_ca_system_score_gemma":0.0003587284,"threshold_uncertainty_score":0.012093782},"labels":[],"label_agreement":null},{"id":"W2140368641","doi":"10.1002/2014jb011352","title":"Plagioclase preferred orientation and induced seismic anisotropy in mafic igneous rocks","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Bedford Institute of Oceanography; Polytechnique Montréal","funders":"","keywords":"Mafic; Plagioclase; Geology; Gabbro; Pyroxene; Geochemistry; Anorthosite; Layered intrusion; Igneous rock; Amphibole; Ultramafic rock; Petrology; Olivine; Quartz","score_opus":0.03118887681411533,"score_gpt":0.306215153947378,"score_spread":0.2750262771332627,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2140368641","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997503,0.000025500618,0.000055734443,0.0000012579369,1.7573966e-7,7.1403e-7,0.00003645483,0.0000038590088,0.00012594434],"genre_scores_gemma":[0.99982244,0.000015414524,0.00005109169,6.8557705e-7,3.0224496e-7,7.944412e-7,0.000055467386,0.0000014376598,0.000052281404],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999349,0.000007459807,0.000004370522,0.00001840852,0.00001918509,0.000015635822],"domain_scores_gemma":[0.99985945,0.000020209358,0.000053539436,0.000011284088,0.000034220368,0.000021284495],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010281358,0.00021928834,0.00009848143,0.0007453361,0.00010448548,0.00030475127,0.00013379176,0.00011120883,0.00047186794],"category_scores_gemma":[0.00026245043,0.00018955306,0.00007721116,0.00030214555,0.00024932332,0.00011911589,0.00016946181,0.00011729007,0.0000834829],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001802487,0.000014154,0.12398736,0.00003227689,0.000032829044,0.00014964519,0.0002007876,0.00065481465,0.87125856,0.000099137585,0.000021832515,0.0033684429],"study_design_scores_gemma":[0.0000054392867,0.00004944691,0.9352161,0.000003014532,0.000010706051,0.0001234876,0.000117752475,0.0015718144,0.06269955,0.00003655951,0.00016064032,0.0000054819425],"about_ca_topic_score_codex":0.0077712694,"about_ca_topic_score_gemma":0.00779158,"teacher_disagreement_score":0.0077712694,"about_ca_system_score_codex":0.00025361587,"about_ca_system_score_gemma":0.00012007543,"threshold_uncertainty_score":0.015452087},"labels":[],"label_agreement":null},{"id":"W2144529009","doi":"10.1002/2013jb010522","title":"Reply to comment by Denyszyn and Halls (this volume) on “Geological and geophysical observations in the Kane Basin preclude the presence of a major plate boundary in southwestern Nares Strait”","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Geological Survey of Canada","funders":"","keywords":"Geology; Lineation; Archipelago; Structural basin; Plate tectonics; Orogeny; Bay; Paleontology; Paleogene; Oceanography; Geomorphology; Tectonics","score_opus":0.058576674850022895,"score_gpt":0.2926193405241478,"score_spread":0.2340426656741249,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2144529009","genre_codex":"commentary","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":"commentary","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00020013866,0.0009805545,0.00009975541,0.965465,0.03263835,0.000007283587,0.000104986575,0.00003841269,0.00046548742],"genre_scores_gemma":[0.0018911051,0.00063434645,0.00011041921,0.96640044,0.02914347,0.000029046665,0.00004257617,0.000035432327,0.0017131144],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99669844,0.0007157165,0.00045962248,0.000772373,0.0010029757,0.00035088713],"domain_scores_gemma":[0.98120016,0.011069932,0.0012297643,0.00070455484,0.004266549,0.0015289922],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.007505354,0.0011564316,0.001751341,0.0010015201,0.0042535733,0.0042532436,0.0044856267,0.03796179,0.009488043],"category_scores_gemma":[0.031863812,0.001281568,0.0013802903,0.0014200724,0.0060019367,0.0070244563,0.003529585,0.04817246,0.009029973],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019269606,0.000005843889,0.00013656022,0.00003010678,0.0000067164365,0.00006094719,0.000112975446,0.000020127445,0.00004572559,0.00043454618,0.99769175,0.001435435],"study_design_scores_gemma":[0.00009403023,0.000041317093,0.0025870167,0.00035846914,0.000036398593,0.0003624554,0.0014718154,0.00025440176,0.00053616293,0.005489172,0.9886516,0.00011712992],"about_ca_topic_score_codex":0.011681547,"about_ca_topic_score_gemma":0.015532729,"teacher_disagreement_score":0.03796179,"about_ca_system_score_codex":0.0033037914,"about_ca_system_score_gemma":0.004501697,"threshold_uncertainty_score":0.03969258},"labels":[],"label_agreement":null},{"id":"W2147846751","doi":"10.1002/2014jb010940","title":"Nontrivial decay of aftershock density with distance in Southern California","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Alberta Innovates","keywords":"Aftershock; Exponent; Seismology; Magnitude (astronomy); Geology; Crust; Shock (circulatory); Scale (ratio); Power law; Anisotropy; Geodesy; Physics; Astrophysics; Geophysics; Mathematics; Statistics; Optics","score_opus":0.02044589728389803,"score_gpt":0.27411485476135183,"score_spread":0.2536689574774538,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2147846751","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983962,0.0000834024,0.00029442323,0.00002423605,0.0000015564525,0.000004370394,0.00048157145,0.000024076813,0.0006902114],"genre_scores_gemma":[0.998985,0.000041844363,0.00011870538,0.0000024378628,0.0000019193762,0.0000020626906,0.00065382104,0.0000021999672,0.00019195465],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997979,0.00001960153,0.000012828568,0.00008034267,0.000053331998,0.000036099245],"domain_scores_gemma":[0.99808794,0.00035007202,0.00057327957,0.0002507104,0.00056909554,0.00016894154],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044452611,0.00018532397,0.000316576,0.0015132913,0.00034095536,0.00097102544,0.00043810884,0.00029185574,0.0010804608],"category_scores_gemma":[0.003231566,0.00021130814,0.000116091906,0.001890511,0.00034621943,0.0005652999,0.0004726307,0.0002618251,0.00010646145],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014079551,0.000054208354,0.9424104,0.00007184133,0.00010024617,0.00025988588,0.00051483477,0.031965233,0.0020121718,0.0017885288,0.0014690887,0.019212758],"study_design_scores_gemma":[0.000019684696,0.000034910947,0.9665864,0.0000161628,0.000021929773,0.000073920644,0.000280086,0.030190257,0.00049551995,0.0006318696,0.0016289272,0.000020258294],"about_ca_topic_score_codex":0.107912116,"about_ca_topic_score_gemma":0.10472821,"teacher_disagreement_score":0.107912116,"about_ca_system_score_codex":0.0011689311,"about_ca_system_score_gemma":0.0004414418,"threshold_uncertainty_score":0.21456802},"labels":[],"label_agreement":null},{"id":"W2148357506","doi":"10.1002/2015jb012132","title":"Magneto‐ and cyclostratigraphy in the red clay sequence: New age model and paleoclimatic implication for the eastern Chinese Loess Plateau","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Northwest University; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China; National Science Foundation","keywords":"Cyclostratigraphy; Magnetostratigraphy; Geology; Milankovitch cycles; Loess; Paleontology; Sedimentary rock; Loess plateau; Plateau (mathematics); Monsoon; Stage (stratigraphy); Climatology; East Asian Monsoon; Paleomagnetism; Glacial period","score_opus":0.10311173143345509,"score_gpt":0.3728976296634812,"score_spread":0.26978589823002613,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2148357506","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9892133,0.00018289889,0.0090516005,0.00010321741,0.00000860714,0.000019865785,0.00013392312,0.000058370864,0.0012281493],"genre_scores_gemma":[0.998298,0.000054518,0.0012353094,0.00000799515,0.000007290998,0.000011595004,0.000100754856,0.000008834493,0.00027572614],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99992573,0.000011143051,0.000006927652,0.000029548553,0.000013101429,0.00001355104],"domain_scores_gemma":[0.99987626,0.000021964424,0.00003238744,0.00001272727,0.000028721553,0.00002785629],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039017588,0.00043094452,0.00028255914,0.0011281429,0.00045625956,0.00086915493,0.0008147334,0.0006604613,0.0012032476],"category_scores_gemma":[0.0005780072,0.00023356972,0.0005183865,0.0004746927,0.00043578196,0.0005585004,0.00039679583,0.0002203022,0.00018041188],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023823541,0.00012350347,0.3865341,0.00010698757,0.00019020775,0.0012712416,0.00052172365,0.5636259,0.02265781,0.0062867766,0.00044097478,0.018002648],"study_design_scores_gemma":[0.000027652228,0.000046964287,0.03967409,0.00001068523,0.00006349845,0.00014372717,0.000084551524,0.9574788,0.0005847066,0.0015027634,0.00036387827,0.000018613013],"about_ca_topic_score_codex":0.018770242,"about_ca_topic_score_gemma":0.009865858,"teacher_disagreement_score":0.018770242,"about_ca_system_score_codex":0.000982612,"about_ca_system_score_gemma":0.00079291605,"threshold_uncertainty_score":0.037321985},"labels":[],"label_agreement":null},{"id":"W2148773537","doi":"10.1002/2015jb012161","title":"Precise relative locations for earthquakes in the northeast Pacific region","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Boettcher Foundation; Los Alamos National Laboratory; National Nuclear Security Administration; U.S. Geological Survey; U.S. Department of Energy; Defense Threat Reduction Agency; National Science Foundation","keywords":"Seismology; Induced seismicity; Geology; Transform fault; Submarine pipeline; Pacific Plate; Fault (geology); Rayleigh wave; Seismogram; Fracture zone; Slip (aerodynamics); Magnitude (astronomy); Subduction; Tectonics; Surface wave; Oceanography","score_opus":0.12257543922742516,"score_gpt":0.3513815990130373,"score_spread":0.22880615978561214,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2148773537","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99730706,0.0000786008,0.0011310143,0.00001617984,0.0000032119522,0.0000043524487,0.0004918705,0.00005212039,0.00091561145],"genre_scores_gemma":[0.9983354,0.00003172695,0.0010781044,0.0000017905113,0.0000015212677,0.0000027373133,0.00040432962,0.000004830836,0.00013964172],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999442,0.0000058199057,0.000003720323,0.000021471753,0.000016888045,0.000007838197],"domain_scores_gemma":[0.999752,0.000051538056,0.00006726927,0.000022512948,0.00008191063,0.000024855191],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020139648,0.00016002556,0.00010411132,0.0006413052,0.00022608662,0.00034038248,0.0002190973,0.00014512826,0.00055552466],"category_scores_gemma":[0.00085615437,0.00011569517,0.00010212149,0.0006575794,0.0001719684,0.00024033815,0.00022219591,0.00015901028,0.00007077358],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018777692,0.000036598685,0.884745,0.00009144399,0.00010014253,0.00023339594,0.00042944506,0.054459777,0.019971816,0.00062200555,0.0006665062,0.038456168],"study_design_scores_gemma":[0.000013859912,0.000024866249,0.9466385,0.000016180298,0.000024702735,0.00006370326,0.0001675065,0.04929319,0.002745785,0.000080498445,0.0009142022,0.000017031065],"about_ca_topic_score_codex":0.103427984,"about_ca_topic_score_gemma":0.14805862,"teacher_disagreement_score":0.103427984,"about_ca_system_score_codex":0.0006114877,"about_ca_system_score_gemma":0.00059904234,"threshold_uncertainty_score":0.20565194},"labels":[],"label_agreement":null},{"id":"W2148933774","doi":"10.1002/jgrb.50102","title":"Subcontinental sinking slab remnants in a spherical geometry mantle model","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"","keywords":"Slab; Geology; Mantle (geology); Transition zone; Slab window; Subduction; Lithosphere; Mantle wedge; Geophysics; Mantle convection; Seismology; Tectonics; Oceanic crust","score_opus":0.03614595234854423,"score_gpt":0.3067936215938322,"score_spread":0.270647669245288,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2148933774","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.700446,0.002061153,0.18720952,0.003525955,0.00019115032,0.00016824101,0.004458964,0.0014439949,0.100495],"genre_scores_gemma":[0.96990687,0.0005709457,0.010122335,0.00024728538,0.00008244941,0.00014543759,0.0008112844,0.00022173116,0.017891675],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998851,0.00003368671,0.0000064030933,0.000025661982,0.000017633638,0.000031446605],"domain_scores_gemma":[0.99961334,0.00010687629,0.00006926297,0.000048124522,0.00006591997,0.000096562246],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038856492,0.0008551331,0.0008124537,0.0007185322,0.0007611974,0.0016397326,0.0036370493,0.002255202,0.00556364],"category_scores_gemma":[0.0010813737,0.0007545304,0.0017797779,0.0007559021,0.0011879627,0.0012476649,0.0016255334,0.0008602434,0.0012641829],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007215889,0.00002242856,0.0011111046,0.00002857094,0.000038112335,0.00023456213,0.000100819285,0.96138257,0.0013929744,0.03382219,0.00070191,0.0010926112],"study_design_scores_gemma":[0.00003792387,0.000013512515,0.0004416613,0.0000055353166,0.000017773998,0.000032734875,0.000031241707,0.9937197,0.000051543164,0.0051510194,0.0004857607,0.000011687585],"about_ca_topic_score_codex":0.059379075,"about_ca_topic_score_gemma":0.018260922,"teacher_disagreement_score":0.059379075,"about_ca_system_score_codex":0.0016227228,"about_ca_system_score_gemma":0.0011071265,"threshold_uncertainty_score":0.11806691},"labels":[],"label_agreement":null},{"id":"W2150777094","doi":"10.1002/2014jb011084","title":"Crustal deformation and stress transfer during a propagating earthquake sequence: The 2013 Cook Strait sequence, central New Zealand","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"Canadian Space Agency; Ministry of Economy, Trade and Industry; National Aeronautics and Space Administration","keywords":"Geology; Sinistral and dextral; Seismology; Foreshock; Bay; Tectonics; Geodesy; Slip (aerodynamics); Aftershock; Oceanography","score_opus":0.03960477484436853,"score_gpt":0.2931846881017314,"score_spread":0.2535799132573629,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2150777094","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989077,0.000034462802,0.000037686455,0.000021970494,0.0000017194283,0.000011691912,0.00036164562,0.000004225328,0.0006188567],"genre_scores_gemma":[0.99922,0.00007296852,0.00006861743,0.000005054369,0.00000170241,0.000008051619,0.00030943716,0.0000023047078,0.00031183587],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999033,0.000004697367,0.000009493577,0.000023700115,0.000033674347,0.000025038473],"domain_scores_gemma":[0.9996265,0.000020902015,0.00015476713,0.000016900094,0.00011733407,0.000063527696],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016365295,0.00033182578,0.00024141779,0.0010557717,0.0005462403,0.00073406484,0.00027990632,0.00028735143,0.0015415268],"category_scores_gemma":[0.0009508645,0.00022514162,0.00021699566,0.0014819207,0.00052027917,0.0003502365,0.00050411705,0.00027391693,0.00020928998],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004728461,0.00012599498,0.93709254,0.0001596135,0.00018623623,0.0016116648,0.0066202353,0.0031933645,0.023039429,0.00018344946,0.0015876509,0.02572698],"study_design_scores_gemma":[0.0000034508244,0.000013074185,0.99903274,0.0000053102635,0.0000059280173,0.000032309606,0.00038902217,0.00026891739,0.00006968374,0.000007248668,0.00016806768,0.0000042251118],"about_ca_topic_score_codex":0.6434913,"about_ca_topic_score_gemma":0.76517963,"teacher_disagreement_score":0.6434913,"about_ca_system_score_codex":0.0023332217,"about_ca_system_score_gemma":0.001358687,"threshold_uncertainty_score":0.71721643},"labels":[],"label_agreement":null},{"id":"W2151391821","doi":"10.1002/2014jb011263","title":"Characteristics of fluid‐induced resonances observed during microseismic monitoring","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary; University of Alberta","funders":"","keywords":"Resonance (particle physics); Hydraulic fracturing; Supercritical fluid; Fluid dynamics; Mechanics; Slurry; Volumetric flow rate; Microseism; Chemistry; Materials science; Geology; Petroleum engineering; Physics; Atomic physics; Seismology; Composite material","score_opus":0.060617172005796964,"score_gpt":0.30900068509845197,"score_spread":0.248383513092655,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2151391821","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9926125,0.000025310079,0.0065982426,0.000013167388,0.00000384452,0.000013183521,0.00010177642,0.00010966238,0.0005224059],"genre_scores_gemma":[0.9992538,0.000006882558,0.0005820488,0.000002223384,0.0000016446224,0.0000057284074,0.000048146223,0.000008787341,0.00009079377],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998481,0.000021548296,0.000007681076,0.000038578866,0.000056322067,0.000027756752],"domain_scores_gemma":[0.999345,0.0003385951,0.0000982222,0.00004502394,0.00011440773,0.000058775462],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032700048,0.00023715633,0.00023335335,0.0008541641,0.00019453879,0.00015985887,0.00030415072,0.00047337465,0.0007733882],"category_scores_gemma":[0.0009137688,0.00013929843,0.00017152166,0.00030989823,0.00031015184,0.00022268138,0.00022977206,0.00027454706,0.00014031652],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011559263,0.00020786989,0.07297917,0.00015586264,0.00007958286,0.0009245033,0.001176802,0.0119984755,0.8790811,0.00046894175,0.0003445889,0.031427335],"study_design_scores_gemma":[0.00006615001,0.0008926066,0.6404733,0.00003609667,0.000084847205,0.0005718414,0.00063439086,0.13506366,0.22026165,0.0003805592,0.0014339188,0.00010097432],"about_ca_topic_score_codex":0.0009371208,"about_ca_topic_score_gemma":0.00090614305,"teacher_disagreement_score":0.0009371208,"about_ca_system_score_codex":0.00016045368,"about_ca_system_score_gemma":0.00007803762,"threshold_uncertainty_score":0.0025872588},"labels":[],"label_agreement":null},{"id":"W2151877576","doi":"10.1002/2014jb011760","title":"Structural controls on the emission of magmatic carbon dioxide gas, Long Valley Caldera, USA","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; McGill University; U.S. Geological Survey; University of Toronto; Geological Society of America","keywords":"Caldera; Geology; Volcano; Hydrothermal circulation; Sedimentary rock; Geochemistry; Induced seismicity; Carbon dioxide; Dome (geology); Fault (geology); Geomorphology; Seismology; Chemistry","score_opus":0.05489561222332626,"score_gpt":0.30333928945799443,"score_spread":0.24844367723466818,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2151877576","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99929106,0.00005993204,0.000029885667,0.000029896271,7.816887e-7,0.0000021237925,0.00012177715,0.0000027554595,0.0004616875],"genre_scores_gemma":[0.99951327,0.000043695276,0.000063024796,0.000018473007,0.0000015212189,0.0000024787423,0.00016310839,0.0000014342932,0.00019291563],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999206,0.000009848345,0.000002710742,0.000024687672,0.000021908932,0.000020147954],"domain_scores_gemma":[0.9997714,0.00003259381,0.00006294453,0.000010393799,0.0000756671,0.000047003345],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012747357,0.0001377363,0.00010985362,0.0005715837,0.0004487579,0.00052495324,0.00031433636,0.00023531547,0.00060387136],"category_scores_gemma":[0.000336035,0.0001120396,0.00010588153,0.0005136325,0.00035919895,0.00018015043,0.0003167143,0.00020251585,0.000064903645],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000106151085,0.00004898783,0.9738196,0.000017530294,0.00006406765,0.00022146563,0.000525944,0.000667819,0.01813482,0.00011139019,0.00025907592,0.006023015],"study_design_scores_gemma":[0.0000025570948,0.000012744364,0.9990245,0.0000016419135,0.000004867627,0.000014760151,0.00016833369,0.00026132996,0.00024217754,0.000010349441,0.0002558495,9.5055304e-7],"about_ca_topic_score_codex":0.17223735,"about_ca_topic_score_gemma":0.38915348,"teacher_disagreement_score":0.17223735,"about_ca_system_score_codex":0.0019151816,"about_ca_system_score_gemma":0.0006505567,"threshold_uncertainty_score":0.34246963},"labels":[],"label_agreement":null},{"id":"W2152056882","doi":"10.1002/2013jb010799","title":"The Alps 2: Controls on crustal subduction and (ultra)high‐pressure rock exhumation in Alpine‐type orogens","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Subduction; Crust; Continental crust; Massif; Continental margin; Mantle (geology); Plate tectonics; Metamorphic rock; Convergent boundary; Eclogitization; Tectonics; Petrology; Geophysics; Seismology; Oceanic crust; Geochemistry","score_opus":0.02216846417401748,"score_gpt":0.2782327056785061,"score_spread":0.25606424150448864,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2152056882","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980433,0.000030046585,0.0006562415,0.000035487526,0.0000014382582,0.0000030730955,0.00013349166,0.000032489,0.0010643189],"genre_scores_gemma":[0.9995497,0.000022631122,0.00021804411,0.000005997102,0.0000015971124,0.0000029090254,0.000082178834,0.000007073966,0.00010991773],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99989164,0.000034477867,0.000007220409,0.000027180295,0.000015100769,0.00002423423],"domain_scores_gemma":[0.99975187,0.00009613335,0.000058705595,0.000034544166,0.00002787052,0.000030773306],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029730212,0.00039880042,0.00034820088,0.0003103033,0.00027018122,0.0010987243,0.00048719998,0.0004383503,0.0016759033],"category_scores_gemma":[0.0007900715,0.00023346193,0.0005118618,0.0002807134,0.00050922274,0.0004398354,0.00054581143,0.00030273982,0.0001313225],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042053315,0.0001033141,0.13430999,0.000058569414,0.00014833524,0.00019947234,0.00013816374,0.8308405,0.026124537,0.002376001,0.00016482848,0.0051157847],"study_design_scores_gemma":[0.00012703238,0.000105728344,0.09730047,0.000009832552,0.000053117637,0.000055680503,0.00013293746,0.8961685,0.004613077,0.00081772247,0.00059061265,0.000025263078],"about_ca_topic_score_codex":0.027805394,"about_ca_topic_score_gemma":0.011457181,"teacher_disagreement_score":0.027805394,"about_ca_system_score_codex":0.00092056923,"about_ca_system_score_gemma":0.0004090581,"threshold_uncertainty_score":0.055287063},"labels":[],"label_agreement":null},{"id":"W2154330854","doi":"10.1002/2014jb011712","title":"Effect of halite coatings on thermal infrared spectra","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Canadian Space Agency; Jet Propulsion Laboratory","keywords":"Halite; Mineralogy; Coating; Infrared spectroscopy; Substrate (aquarium); Infrared; Spectroscopy; Optics; Materials science; Geology; Chemistry; Composite material; Physics","score_opus":0.04299644469432544,"score_gpt":0.34678960005027265,"score_spread":0.3037931553559472,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2154330854","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976675,0.00022274102,0.001035549,0.000019883479,0.000008863553,0.0000072098946,0.00009375489,0.00006300038,0.0008815566],"genre_scores_gemma":[0.99797803,0.00013867197,0.0011322129,0.000030119956,0.0000028389832,0.0000066561206,0.00008769049,0.000045415065,0.00057838013],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9997571,0.000027833135,0.000010594049,0.00005229644,0.000093890616,0.000058235055],"domain_scores_gemma":[0.99933016,0.00027707935,0.000103459606,0.000053747895,0.00018178587,0.000053813343],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024131055,0.00037791362,0.00020467624,0.0002590782,0.00018762221,0.0004899197,0.00022366126,0.0002566235,0.0016513664],"category_scores_gemma":[0.000801133,0.00024455859,0.00025873852,0.00020438663,0.00032412237,0.00021652177,0.0002327374,0.00039110915,0.00023534441],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015170495,0.00001118736,0.00092370884,0.000032861135,0.000013073687,0.00003625417,0.000043549,0.00029745305,0.9970902,0.000017151653,0.000039987553,0.0013428284],"study_design_scores_gemma":[0.000007711634,0.00009605978,0.0075533604,0.0000033858541,0.000017414155,0.00003505833,0.00006114118,0.0029730294,0.98894274,0.000013328347,0.00028720195,0.000009608529],"about_ca_topic_score_codex":0.003026226,"about_ca_topic_score_gemma":0.0025917077,"teacher_disagreement_score":0.003026226,"about_ca_system_score_codex":0.00035908734,"about_ca_system_score_gemma":0.00013118258,"threshold_uncertainty_score":0.006017208},"labels":[],"label_agreement":null},{"id":"W2155928202","doi":"10.1002/2014jb011596","title":"Volcanic tremor and frequency gliding during dike intrusions at Kılauea—A tale of three eruptions","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Institute for Advanced Research","keywords":"Dike; Geology; Magma; Seismology; Volcano; Intrusion; Lava; Impact crater; Phase (matter); Petrology; Physics; Geochemistry","score_opus":0.07803422778911674,"score_gpt":0.3218896628652319,"score_spread":0.24385543507611518,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2155928202","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994117,0.000032509448,0.000049756465,0.0000075816133,0.0000021992241,0.0000051515676,0.00011098861,0.000005285505,0.00037487852],"genre_scores_gemma":[0.99915063,0.000028117927,0.00012714656,0.000010535629,0.000006320687,0.000010151,0.00043162043,0.0000033488275,0.00023217987],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998723,0.0000063250714,0.000010283458,0.000038772225,0.00003247763,0.000039879953],"domain_scores_gemma":[0.9996575,0.000039578088,0.000087648696,0.000023390789,0.00007403241,0.00011782954],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021061541,0.00032461842,0.00040715604,0.0014155377,0.0006662469,0.0005725523,0.00033582907,0.00070780824,0.0006902529],"category_scores_gemma":[0.00032580463,0.00027573959,0.00035376896,0.00082337117,0.00041747317,0.00035378904,0.0006830378,0.000501783,0.00020051816],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044631315,0.00018788756,0.9319668,0.000065933986,0.00015838597,0.0011286894,0.0018063517,0.0006202655,0.054033395,0.000047780843,0.0002593219,0.009278889],"study_design_scores_gemma":[0.0000024282006,0.000027908958,0.9989839,0.0000023684274,0.000008998059,0.00006125002,0.00025718013,0.00016864388,0.0003440607,0.0000032948847,0.00013491446,0.0000049163586],"about_ca_topic_score_codex":0.009860242,"about_ca_topic_score_gemma":0.034682233,"teacher_disagreement_score":0.009860242,"about_ca_system_score_codex":0.00050691393,"about_ca_system_score_gemma":0.00024262229,"threshold_uncertainty_score":0.019605696},"labels":[],"label_agreement":null},{"id":"W2156395869","doi":"10.1002/jgrb.50325","title":"A hydrologic model for the uppermost oceanic crust constrained by temperature estimates from carbonate minerals","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Aquifer; Geology; Outcrop; Carbonate; Geochemistry; Crust; Petrology; Aquifer test; Carbonate rock; Geomorphology; Groundwater; Sedimentary rock; Groundwater recharge; Geotechnical engineering","score_opus":0.039133953535944135,"score_gpt":0.30049901367181253,"score_spread":0.2613650601358684,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2156395869","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.89494693,0.00020607315,0.08955703,0.00078174414,0.000030983236,0.00006638146,0.0015970584,0.00026189108,0.012551911],"genre_scores_gemma":[0.9935527,0.000108872584,0.0030636261,0.000034193974,0.00001291901,0.000046201483,0.00030053372,0.000036557234,0.0028443313],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989307,0.000023066836,0.000006905171,0.000041563406,0.000012518564,0.000022875849],"domain_scores_gemma":[0.9996599,0.00012656637,0.00008675989,0.000029237775,0.000046201294,0.00005126195],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037912803,0.0005298258,0.0003210574,0.00050992245,0.00043015054,0.0013941275,0.0014669242,0.0008182988,0.00276277],"category_scores_gemma":[0.0012221204,0.0006673193,0.00071961223,0.00056218967,0.00087689364,0.0010729245,0.00068665127,0.000581211,0.00036418068],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000029712834,0.000015048185,0.0047727814,0.0000068071136,0.000018341245,0.000060027127,0.000023967668,0.98981804,0.0011649721,0.0030471736,0.00012496406,0.00091813656],"study_design_scores_gemma":[0.000020708272,0.0000073657575,0.0017424067,0.000002404435,0.000008408782,0.000010653455,0.000014597434,0.9963909,0.00012746801,0.0014911983,0.00017692693,0.0000070252377],"about_ca_topic_score_codex":0.06599459,"about_ca_topic_score_gemma":0.027457071,"teacher_disagreement_score":0.06599459,"about_ca_system_score_codex":0.0014264502,"about_ca_system_score_gemma":0.0014893174,"threshold_uncertainty_score":0.13122094},"labels":[],"label_agreement":null},{"id":"W2156568407","doi":"10.1002/2015jb012195","title":"Magnitudes and moment‐duration scaling of low‐frequency earthquakes beneath southern Vancouver Island","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":123,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Scaling; Moment magnitude scale; Geodesy; Attenuation; Waveform; Seismology; Magnitude (astronomy); Moment (physics); Geology; Physics; Slip (aerodynamics); Exponential decay; Geometry; Optics; Mathematics; Astrophysics; Voltage; Classical mechanics","score_opus":0.0492726265220276,"score_gpt":0.30627212708802154,"score_spread":0.25699950056599397,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2156568407","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99757856,0.000032507403,0.00024604975,0.000014738845,0.0000016693408,0.000004736075,0.00075999787,0.000018468168,0.0013433258],"genre_scores_gemma":[0.9985,0.000027010667,0.00019997144,0.0000028386103,0.0000012746742,0.0000029125847,0.00086104596,0.000005714781,0.00039919923],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999897,0.0000063251914,0.0000061523033,0.00002646069,0.00004188848,0.00002220604],"domain_scores_gemma":[0.99938214,0.00009016076,0.00009878076,0.000037386297,0.00027310263,0.00011844187],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000105535786,0.00016288683,0.00015941774,0.0011892738,0.00032985542,0.0008669304,0.00027920588,0.00021375198,0.0014935966],"category_scores_gemma":[0.0011706962,0.00019097679,0.00010606222,0.0011161668,0.00017515403,0.00013230754,0.0003326921,0.00016944032,0.00032928513],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009155951,0.000032164815,0.947534,0.000044989854,0.00007056081,0.00012814814,0.00050519063,0.0038174528,0.017537698,0.00010833247,0.000526253,0.029603595],"study_design_scores_gemma":[0.0000013324192,0.0000041118815,0.99748224,0.00000308785,0.0000038576527,0.000016366988,0.00010666675,0.001963713,0.0002004921,0.000012468079,0.00020255543,0.0000031233817],"about_ca_topic_score_codex":0.41433614,"about_ca_topic_score_gemma":0.60367256,"teacher_disagreement_score":0.58566386,"about_ca_system_score_codex":0.0008954766,"about_ca_system_score_gemma":0.0006252865,"threshold_uncertainty_score":0.82384884},"labels":[],"label_agreement":null},{"id":"W2156721705","doi":"10.1002/2014jb011707","title":"Viscoelastic relaxation following subduction earthquakes and its effects on afterslip determination","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":153,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Viscoelasticity; Geology; Seismology; Subduction; Trench; Rheology; Deformation (meteorology); Geodesy; Tectonics; Physics","score_opus":0.050057334766599515,"score_gpt":0.3268103994822256,"score_spread":0.2767530647156261,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2156721705","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989478,0.000067877954,0.0005276833,0.00001410739,0.0000021105873,0.000003160291,0.00004558101,0.000020074638,0.00037155388],"genre_scores_gemma":[0.9997677,0.00003317969,0.00008708758,0.000002828025,0.0000011427016,0.0000014031096,0.00004152464,0.0000037569396,0.000061384075],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998838,0.000022289172,0.000011905358,0.000030286341,0.000017997329,0.000033751046],"domain_scores_gemma":[0.99829453,0.0007791436,0.00044879803,0.00018097059,0.00016624272,0.00013028424],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005631743,0.0004179432,0.00026012765,0.0010347777,0.00022132944,0.00057935156,0.00022910966,0.00025031273,0.0007000253],"category_scores_gemma":[0.0024804731,0.0002342593,0.00036023906,0.0005834083,0.00027586106,0.00050090416,0.0005750256,0.00032419807,0.00015434071],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00097138656,0.00023455848,0.7557946,0.00014330931,0.00026652924,0.001319386,0.0007585163,0.064434886,0.12152801,0.00041113602,0.00028357445,0.053854104],"study_design_scores_gemma":[0.000008740544,0.00015467829,0.89221954,0.000020088428,0.00006407854,0.00010361807,0.00025345632,0.09879367,0.007997467,0.00014519875,0.00020968146,0.000029841287],"about_ca_topic_score_codex":0.004562883,"about_ca_topic_score_gemma":0.003946207,"teacher_disagreement_score":0.004562883,"about_ca_system_score_codex":0.00023803211,"about_ca_system_score_gemma":0.00020780085,"threshold_uncertainty_score":0.009072661},"labels":[],"label_agreement":null},{"id":"W2159614822","doi":"10.1002/jgrb.50208","title":"Antarctic contribution to sea level rise observed by GRACE with improved GIA correction","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":261,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"National Aeronautics and Space Administration","keywords":"Post-glacial rebound; Geology; Ice sheet; Geodesy; Antarctic ice sheet; Lithosphere; Climatology; Sea ice; Geomorphology; Cryosphere; Paleontology; Tectonics","score_opus":0.0587292035796822,"score_gpt":0.2940973550038323,"score_spread":0.23536815142415007,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2159614822","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9053801,0.0014698632,0.030897561,0.0016058017,0.00045807546,0.00007874175,0.033523154,0.0091244,0.017462293],"genre_scores_gemma":[0.94555974,0.0006578511,0.021598738,0.00025835188,0.00026414983,0.000051056028,0.028399445,0.0008912677,0.002319402],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99937767,0.00012237718,0.000059307622,0.00013102949,0.00023267511,0.00007692571],"domain_scores_gemma":[0.9990779,0.00007764191,0.00016053066,0.00034648206,0.00031022663,0.000027131122],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009394403,0.00082094263,0.00045653933,0.0011900925,0.00017674227,0.0007734056,0.0006066019,0.0003172985,0.001035216],"category_scores_gemma":[0.0031369107,0.00024461639,0.00092101976,0.0028419069,0.00018053819,0.0006653573,0.00074034726,0.0005017347,0.0009044842],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008696034,0.00015092338,0.40700597,0.00030459373,0.0014436714,0.000539853,0.00029130303,0.2767197,0.025178852,0.0043561,0.029686963,0.25345254],"study_design_scores_gemma":[0.0001531588,0.000099447956,0.630194,0.000057847545,0.00050013704,0.00032092046,0.000050129478,0.30867922,0.008835625,0.0015359477,0.04943597,0.00013769414],"about_ca_topic_score_codex":0.025419446,"about_ca_topic_score_gemma":0.02809964,"teacher_disagreement_score":0.025419446,"about_ca_system_score_codex":0.0006290447,"about_ca_system_score_gemma":0.00080112915,"threshold_uncertainty_score":0.05054295},"labels":[],"label_agreement":null},{"id":"W2159968103","doi":"10.1002/2014jb011495","title":"Mechanical stability model of progradational carbonate platform margins under tectonic loads: Deformation of Cretaceous carbonate platforms in the Sierra Madre Oriental fold‐thrust belt (east central Mexico)","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"ASTER","funders":"Centro de Investigación Científica y de Educación Superior de Ensenada, Baja California; Geological Society of America","keywords":"Geology; Carbonate platform; Cretaceous; Fold and thrust belt; Fold (higher-order function); Carbonate; Petrology; Foreland basin; Geomorphology; Facies; Structural basin; Paleontology","score_opus":0.08207041450478778,"score_gpt":0.29092863852546036,"score_spread":0.20885822402067258,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2159968103","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97429556,0.00009515207,0.018587003,0.00016891437,0.000012874707,0.000029299832,0.00029437704,0.00010765374,0.006409072],"genre_scores_gemma":[0.9974281,0.000030133777,0.0007766532,0.000009508174,0.0000038326625,0.000025127028,0.00007491358,0.000009864765,0.0016417524],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99995446,0.000008048013,0.0000022118302,0.000012927277,0.00000910595,0.000013267617],"domain_scores_gemma":[0.9999126,0.000026661419,0.000021851876,0.000006963807,0.00002157823,0.000010335945],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016766408,0.00044757518,0.0002884681,0.00054024864,0.00056366913,0.00056872546,0.0007648111,0.0010072619,0.0021027676],"category_scores_gemma":[0.0003625002,0.00031465568,0.00048867136,0.0001984671,0.0005597488,0.00022860126,0.00033729913,0.00024393608,0.00022437592],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004389865,0.00002797837,0.0064262096,0.000013888842,0.000021624237,0.00012258877,0.000057619167,0.9870165,0.003478027,0.001001336,0.00013365643,0.001656631],"study_design_scores_gemma":[0.000006837741,0.000015669952,0.0028210112,0.0000026721366,0.000005299552,0.000008641202,0.000020988939,0.99668485,0.00017374799,0.00015211896,0.00010504904,0.0000031223585],"about_ca_topic_score_codex":0.058213588,"about_ca_topic_score_gemma":0.023912303,"teacher_disagreement_score":0.058213588,"about_ca_system_score_codex":0.00096941757,"about_ca_system_score_gemma":0.0006903221,"threshold_uncertainty_score":0.11574948},"labels":[],"label_agreement":null},{"id":"W2160244801","doi":"10.1002/2013jb010692","title":"Shear wave seismic interferometry for lithospheric imaging: Application to southern Mexico","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Shell (Canada)","funders":"","keywords":"Geology; Seismic interferometry; Seismology; Shear zone; Interferometry; Shear (geology); Receiver function; Lithosphere; Passive seismic; Seismometer; Subduction; Remote sensing; Geodesy; Optics; Tectonics; Physics; Petrology","score_opus":0.025738762500126203,"score_gpt":0.30767493412286495,"score_spread":0.28193617162273876,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2160244801","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99233466,0.00010428735,0.0054268646,0.000062138926,0.000003643518,0.000030546104,0.00048962777,0.00015528504,0.0013927729],"genre_scores_gemma":[0.98198456,0.0001763413,0.016853457,0.0000067007322,0.000006628726,0.00002728105,0.00045580734,0.000015052384,0.00047424],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999702,0.0000058989704,0.0000016181641,0.000008483976,0.000008280714,0.0000055014925],"domain_scores_gemma":[0.99990094,0.000030513955,0.00001874416,0.000014295085,0.000027087985,0.0000084514995],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001642495,0.00019136177,0.00011171806,0.000487334,0.00030275944,0.0002814096,0.00018432352,0.00014862107,0.0007708975],"category_scores_gemma":[0.00034103662,0.000093437186,0.00011400089,0.00067813165,0.000099144214,0.000113973176,0.00018558885,0.00012888109,0.000071763294],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00075387454,0.0003889927,0.49998677,0.00013986106,0.00013874407,0.0009834385,0.0006027164,0.043282926,0.15722148,0.0010971191,0.0016027238,0.29380137],"study_design_scores_gemma":[0.00017835567,0.00022496418,0.8490729,0.000019838151,0.00009223842,0.00017880886,0.00052168715,0.12591122,0.01899076,0.000414362,0.0043705623,0.000024346067],"about_ca_topic_score_codex":0.038547095,"about_ca_topic_score_gemma":0.05941848,"teacher_disagreement_score":0.038547095,"about_ca_system_score_codex":0.0002637131,"about_ca_system_score_gemma":0.00033077117,"threshold_uncertainty_score":0.076645434},"labels":[],"label_agreement":null},{"id":"W2160303828","doi":"10.1002/2014jb011018","title":"The building and stabilization of an Archean Craton in the Superior Province, Canada, from a heat flow perspective","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Craton; Geology; Lithosphere; Terrane; Archean; Crust; Petrology; Mantle (geology); Geochemistry; Tectonics; Earth science; Geophysics; Seismology","score_opus":0.016867444384724654,"score_gpt":0.273350722168111,"score_spread":0.25648327778338637,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2160303828","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.995262,0.00021529704,0.00012652291,0.00006753856,0.00000279974,0.000009993301,0.00049296784,0.000016806804,0.003806007],"genre_scores_gemma":[0.9985806,0.00007739668,0.00017958597,0.0000075407534,9.607339e-7,0.0000018130629,0.00016763201,0.000003346004,0.0009811615],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987125,0.000003994003,0.0000031103605,0.000027451466,0.00004216475,0.000051950996],"domain_scores_gemma":[0.99979573,0.000007246681,0.000020127078,0.000008428196,0.00012603238,0.00004244117],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001253961,0.00026356932,0.00020932789,0.0013758275,0.0019570375,0.00095492916,0.0005447499,0.00023855582,0.0016161897],"category_scores_gemma":[0.00044301973,0.00022404095,0.00023007614,0.0014514059,0.0013114843,0.00019707976,0.00063764653,0.00021963903,0.00014263939],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035168885,0.000036077145,0.9013188,0.00015691522,0.00011904896,0.0010093187,0.0038408998,0.012311055,0.03335629,0.0029240581,0.0014313008,0.04314465],"study_design_scores_gemma":[0.0000042888887,0.000012280883,0.9938041,0.000014601055,0.000011630157,0.000047043108,0.0008731628,0.0020045335,0.00053645327,0.00009196865,0.0025928374,0.000007018897],"about_ca_topic_score_codex":0.98867536,"about_ca_topic_score_gemma":0.99401784,"teacher_disagreement_score":0.01843661,"about_ca_system_score_codex":0.01843661,"about_ca_system_score_gemma":0.01272777,"threshold_uncertainty_score":0.1337676},"labels":[],"label_agreement":null},{"id":"W2161504423","doi":"10.1002/2014jb011386","title":"Measurements of the changing wave velocities of sand during the formation and dissociation of disseminated methane hydrate","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Hydrate; Methane; Dissociation (chemistry); Clathrate hydrate; Chemical physics; Saturation (graph theory); Geology; Chemistry; Mineralogy; Physical chemistry; Organic chemistry","score_opus":0.05730580346969213,"score_gpt":0.30845598766145466,"score_spread":0.25115018419176255,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2161504423","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989857,0.000021473134,0.00071040523,0.0000027844924,0.0000011380421,0.0000034700363,0.000051434843,0.000008023908,0.00021559041],"genre_scores_gemma":[0.9988889,0.000021379168,0.0006684276,0.000002528988,5.0403713e-7,0.0000041041385,0.00008061784,0.000003643834,0.00033000772],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999342,0.0000040423397,0.0000036851368,0.000012603629,0.00003082871,0.00001452855],"domain_scores_gemma":[0.9998703,0.000024582076,0.00003541774,0.000011359976,0.000033178443,0.000025242804],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000099789955,0.00012231564,0.00010906713,0.00023609643,0.00019098427,0.00019734378,0.00013959974,0.00009843703,0.000520204],"category_scores_gemma":[0.00022067725,0.0001233494,0.00008550715,0.00015482609,0.00032391603,0.00015574797,0.00018280497,0.00027254462,0.00009594986],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000112065085,0.000008774,0.008815009,0.0000098083065,0.0000039221763,0.000037354403,0.000098596676,0.00012511591,0.9892833,0.000035908033,0.000011105261,0.0014591316],"study_design_scores_gemma":[0.0000062588674,0.00020813657,0.20126775,0.0000030321462,0.000009389466,0.00008512429,0.0002454306,0.0022207268,0.79542243,0.000033707867,0.00048896176,0.000009055321],"about_ca_topic_score_codex":0.001901445,"about_ca_topic_score_gemma":0.003556642,"teacher_disagreement_score":0.001901445,"about_ca_system_score_codex":0.00022071556,"about_ca_system_score_gemma":0.00012740625,"threshold_uncertainty_score":0.0037807822},"labels":[],"label_agreement":null},{"id":"W2162981629","doi":"10.1002/2013jb010834","title":"Controls on spatial and temporal evolution of prism faulting and relationships to plate boundary slip offshore north‐central Sumatra","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; Bundesministerium für Bildung und Forschung; Natural Environment Research Council; University of Southampton; Sight Research UK","keywords":"Geology; Seismology; Forearc; Submarine pipeline; Slip (aerodynamics); Fault (geology); Accretionary wedge; Strike-slip tectonics; Plate tectonics; Ridge; Subduction; Tectonics; Paleontology","score_opus":0.03821904790724438,"score_gpt":0.29269940779125353,"score_spread":0.25448035988400913,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2162981629","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994393,0.000020517946,0.000025310297,0.000012689307,8.091875e-7,8.6407334e-7,0.00009146353,0.000002517696,0.00040650225],"genre_scores_gemma":[0.9997161,0.00002055928,0.00002290249,0.0000029889895,7.6378905e-7,0.0000018959752,0.00007693679,0.00000163617,0.00015620592],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998816,0.000024157933,0.000010125746,0.000043793956,0.000013991664,0.00002634672],"domain_scores_gemma":[0.9993824,0.00014885639,0.0002405817,0.0000482288,0.00008214596,0.000097831355],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021473206,0.00016895325,0.00016229988,0.00072318746,0.00022588429,0.00062512263,0.00018720762,0.00017654587,0.0023124162],"category_scores_gemma":[0.0010569688,0.00018296053,0.00011338089,0.0006236124,0.00048287827,0.00029258765,0.0004906413,0.00019867838,0.00024778294],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000333543,0.00007615528,0.93148446,0.00005721735,0.00009036886,0.000730563,0.0014314463,0.0027650697,0.05065987,0.00032078516,0.00021536405,0.011835194],"study_design_scores_gemma":[0.0000015547014,0.0000075468324,0.99913305,0.000002211527,0.0000033218844,0.00003089389,0.00023200114,0.00031620867,0.0001664149,0.000019961268,0.00008504531,0.0000017741977],"about_ca_topic_score_codex":0.015547384,"about_ca_topic_score_gemma":0.032474313,"teacher_disagreement_score":0.015547384,"about_ca_system_score_codex":0.0005634307,"about_ca_system_score_gemma":0.00020891875,"threshold_uncertainty_score":0.03091377},"labels":[],"label_agreement":null},{"id":"W2164032923","doi":"10.1002/2013jb010931","title":"Welding of pyroclastic conduit infill: A mechanism for cyclical explosive eruptions","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Pyroclastic rock; Geology; Explosive eruption; Peléan eruption; Volcano; Tephra; Pumice; Electrical conduit; Vulcanian eruption; Petrology; Impact crater; Breccia; Seismology","score_opus":0.06081908463435662,"score_gpt":0.32643782633903484,"score_spread":0.26561874170467825,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2164032923","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99694246,0.00011846934,0.0019920818,0.000032872314,0.0000034077977,0.000011640034,0.00006396008,0.00008131895,0.00075365877],"genre_scores_gemma":[0.99929035,0.000023607718,0.00050732726,0.0000055396777,0.0000011697255,0.0000033440103,0.000024583049,0.0000056019317,0.00013839452],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998951,0.0000059991858,0.000005107867,0.000044830707,0.000026995733,0.000022005137],"domain_scores_gemma":[0.99973863,0.000057585454,0.00009648762,0.00004284872,0.000036270852,0.000028156137],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018087402,0.00023944017,0.00018678434,0.0007247346,0.00042608214,0.00078544964,0.0006698189,0.0004427753,0.000965193],"category_scores_gemma":[0.00062200194,0.00029339746,0.00014660186,0.0003900145,0.00068377436,0.00042256227,0.00037116936,0.00026070417,0.00013305234],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018410779,0.00013947944,0.22887608,0.00017093895,0.00007320774,0.0023684476,0.0010071052,0.0233047,0.72160256,0.0023663559,0.00033895302,0.019568156],"study_design_scores_gemma":[0.000026891004,0.00015998038,0.7178401,0.00004175806,0.000054642733,0.0017371794,0.0008850949,0.13900994,0.13619196,0.0012715247,0.002732834,0.000048095284],"about_ca_topic_score_codex":0.0050848373,"about_ca_topic_score_gemma":0.00598327,"teacher_disagreement_score":0.0050848373,"about_ca_system_score_codex":0.00054772355,"about_ca_system_score_gemma":0.00019178975,"threshold_uncertainty_score":0.0101104975},"labels":[],"label_agreement":null},{"id":"W2164689425","doi":"10.1002/2014jb011739","title":"The oceanic crustal structure at the extinct, slow to ultraslow Labrador Sea spreading center","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University; Geological Survey of Canada","funders":"Natural Resources Canada; Government of Canada","keywords":"Geology; Crust; Oceanic crust; Lithosphere; Mantle (geology); Seismology; Seafloor spreading; Ridge; Tectonics; Mid-ocean ridge; Seismic tomography; Basement; Seismic refraction; Geophysics; Subduction; Paleontology","score_opus":0.033297136713739676,"score_gpt":0.29275288168724534,"score_spread":0.25945574497350565,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2164689425","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99878174,0.000026958807,0.000059528367,0.0000073960323,3.6134986e-7,0.0000017519918,0.0004283072,0.000016597882,0.0006774016],"genre_scores_gemma":[0.9987978,0.0000191309,0.00014200732,0.0000036281515,5.0290606e-7,0.0000014211907,0.00067820755,0.0000049034097,0.000352381],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994016,0.0000043703035,0.0000033092324,0.000017089835,0.00001511173,0.000019877107],"domain_scores_gemma":[0.99985886,0.000010238913,0.000044589204,0.000016030619,0.00004249768,0.00002775226],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008613435,0.0002624507,0.00010521746,0.0009060472,0.0002717851,0.0004690554,0.00032430165,0.0001471785,0.001358273],"category_scores_gemma":[0.00019143002,0.0001461431,0.0001543516,0.000668479,0.00026846904,0.00017879494,0.000385475,0.00014729421,0.00024730267],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013492389,0.000025134977,0.95112437,0.000027204956,0.00006134983,0.00027760543,0.0007763116,0.0038006927,0.023093933,0.00014859247,0.00044724718,0.020082576],"study_design_scores_gemma":[0.0000022242828,0.000010404053,0.9974771,0.000004629336,0.0000060448674,0.000030065159,0.00017851307,0.0012902914,0.00067812385,0.0000070779984,0.00031235057,0.0000032744426],"about_ca_topic_score_codex":0.28764552,"about_ca_topic_score_gemma":0.45811522,"teacher_disagreement_score":0.7123545,"about_ca_system_score_codex":0.0011931491,"about_ca_system_score_gemma":0.00039238183,"threshold_uncertainty_score":0.57194245},"labels":[],"label_agreement":null},{"id":"W2165793787","doi":"10.1002/2013jb010101","title":"North Cascadia heat flux and fluid flow from gas hydrates: Modeling 3‐D topographic effects","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"Peking University; Ministry of Education of the People's Republic of China; National Natural Science Foundation of China","keywords":"Geology; Seafloor spreading; Fluid dynamics; Clathrate hydrate; Ridge; Petrology; Heat flux; Drilling; Flux (metallurgy); Geomorphology; Volumetric flow rate; Methane; Geophysics; Hydrate; Heat transfer; Mechanics","score_opus":0.01763767852501576,"score_gpt":0.2678284748797946,"score_spread":0.25019079635477887,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2165793787","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99317896,0.00004395669,0.0033192867,0.00011403717,0.000013579281,0.000018237264,0.000562928,0.00037947734,0.0023695],"genre_scores_gemma":[0.9974963,0.00003479172,0.0015609232,0.000010943839,0.0000049249907,0.000018425164,0.00018863518,0.000040863517,0.0006442893],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991274,0.000014939537,0.0000040946707,0.000030960015,0.000016897082,0.000020391008],"domain_scores_gemma":[0.99972266,0.00009849537,0.00003611154,0.00003066627,0.000056581146,0.000055388908],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022303923,0.0006872303,0.00032240484,0.00065507053,0.0006158506,0.00069303287,0.0009847146,0.0010153286,0.0016596058],"category_scores_gemma":[0.00081399386,0.00052405184,0.0009583092,0.0005862064,0.00071626273,0.00026675267,0.00044943878,0.00055983337,0.00022961746],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000047636342,0.000036572223,0.017848179,0.000016492348,0.00003465304,0.00009255089,0.00006161081,0.9782906,0.0018724941,0.000184525,0.00019624384,0.0013184565],"study_design_scores_gemma":[0.000023119594,0.000011315424,0.010078943,0.0000020612558,0.000011223459,0.000009663543,0.000021399184,0.98932236,0.00027442622,0.00006751418,0.00016641854,0.000011619997],"about_ca_topic_score_codex":0.34220526,"about_ca_topic_score_gemma":0.20526262,"teacher_disagreement_score":0.34220526,"about_ca_system_score_codex":0.002672363,"about_ca_system_score_gemma":0.0014002003,"threshold_uncertainty_score":0.68042684},"labels":[],"label_agreement":null},{"id":"W2167822840","doi":"10.1002/2014jb011022","title":"Fluid seepage velocities through marine sediments constrained by a global compilation of interstitial water SO<sub>4</sub><sup>2−</sup>, Mg<sup>2+</sup>, and Ca<sup>2+</sup> profiles","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Drilling; Sediment; Hydrothermal circulation; Oceanic crust; Aquifer; Outcrop; Flux (metallurgy); Basement; Seawater; Advection; Ridge; Geochemistry; Geomorphology; Oceanography; Groundwater; Paleontology; Subduction","score_opus":0.014637711409129395,"score_gpt":0.27311386944772514,"score_spread":0.25847615803859575,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2167822840","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982864,0.000023138324,0.00036577779,0.0000075015123,0.0000011550223,0.0000023547896,0.001020905,0.00004896132,0.00024373642],"genre_scores_gemma":[0.9955634,0.000038098107,0.0007671141,0.000004457895,0.000002177359,0.000006539809,0.0035019554,0.000016339274,0.00010009239],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999256,0.000007613334,0.0000070014958,0.000034211535,0.000010773498,0.00001474333],"domain_scores_gemma":[0.9997801,0.000033162985,0.000078779565,0.00002808929,0.000042585816,0.000037276408],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021266458,0.00058657106,0.00029434136,0.0011088004,0.00016699765,0.0006563425,0.0002042493,0.00030915547,0.00048926845],"category_scores_gemma":[0.00058675226,0.00035231028,0.0005932118,0.0010294641,0.0001918997,0.00040631098,0.0004217174,0.00012224172,0.00016349994],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012728908,0.00003330527,0.94763786,0.000051248422,0.00022727746,0.00016714878,0.00013571758,0.028698772,0.014735553,0.00015502791,0.00035720266,0.0076735923],"study_design_scores_gemma":[0.000013382039,0.00003780563,0.9672522,0.000010265435,0.00005379267,0.0000690119,0.00013410585,0.029306384,0.0023127955,0.0000934276,0.0007013968,0.000015367124],"about_ca_topic_score_codex":0.017605875,"about_ca_topic_score_gemma":0.021915559,"teacher_disagreement_score":0.017605875,"about_ca_system_score_codex":0.00029787523,"about_ca_system_score_gemma":0.0003537327,"threshold_uncertainty_score":0.03500676},"labels":[],"label_agreement":null},{"id":"W2167932491","doi":"10.1002/2015jb012150","title":"Lithological control on gas hydrate saturation as revealed by signal classification of NMR logging data","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"NMR spectroscopy and applications","field":"Physics and Astronomy","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ; U.S. Department of Energy","keywords":"Clathrate hydrate; Hydrate; Saturation (graph theory); Lithology; Well logging; Cluster analysis; Porosity; Mineralogy; Geology; Chemistry; Petroleum engineering; Geotechnical engineering; Petrology; Artificial intelligence; Computer science; Mathematics","score_opus":0.10232990290414432,"score_gpt":0.4476810041241126,"score_spread":0.34535110121996826,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2167932491","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968263,0.000019827572,0.0026280019,0.0000062236427,0.0000014170632,0.000003548127,0.00007939935,0.000043398646,0.00039193427],"genre_scores_gemma":[0.99800545,0.000016616139,0.0017198558,0.0000029753105,0.0000012528908,0.0000032958694,0.00010129986,0.000010926329,0.00013832192],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999001,0.00001438853,0.0000067333576,0.00002718755,0.00003190601,0.000019640922],"domain_scores_gemma":[0.9994665,0.00019469178,0.00009748716,0.000043887798,0.00016136577,0.000036150388],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026156887,0.00015206392,0.00010471979,0.00058240606,0.00014680442,0.00035306966,0.00013790911,0.000102245525,0.0004284406],"category_scores_gemma":[0.0009381992,0.000077837474,0.00006220709,0.0003791582,0.00027549625,0.00022940476,0.00014076452,0.000088338886,0.00009417498],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008824355,0.000051896564,0.105785474,0.000068937916,0.000033347515,0.00016054504,0.0004990751,0.006199932,0.8109536,0.00022353847,0.00014617278,0.07499502],"study_design_scores_gemma":[0.000010421488,0.00014737828,0.7459536,0.000008768076,0.000040728646,0.00013186282,0.00047356376,0.049160637,0.20295936,0.00013400184,0.00094300276,0.000036653248],"about_ca_topic_score_codex":0.005535556,"about_ca_topic_score_gemma":0.0099461945,"teacher_disagreement_score":0.005535556,"about_ca_system_score_codex":0.00016451423,"about_ca_system_score_gemma":0.00019948477,"threshold_uncertainty_score":0.011006653},"labels":[],"label_agreement":null},{"id":"W2181016351","doi":"10.1002/2015jb012228","title":"Variability and origin of seismic anisotropy across eastern Canada: Evidence from shear wave splitting measurements","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; Leverhulme Trust","keywords":"Lithosphere; Geology; Seismic anisotropy; Shear wave splitting; Anisotropy; Geophysics; Mantle (geology); Seismology; Tectonics; Shear (geology); Petrology; Physics","score_opus":0.15346457239793038,"score_gpt":0.3517145771071379,"score_spread":0.1982500047092075,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2181016351","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954899,0.00015058635,0.00017729081,0.000063790314,0.0000029940045,0.000009650415,0.0021985725,0.000015629523,0.0018917315],"genre_scores_gemma":[0.99804723,0.00011294372,0.00017177442,0.00001750215,0.0000016296065,0.0000040110017,0.0012056446,0.0000069417933,0.00043235865],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99948287,0.000027139997,0.000025743118,0.00011496682,0.00018611281,0.00016309829],"domain_scores_gemma":[0.996999,0.00024846164,0.0004171077,0.00015229378,0.0017790308,0.00040412587],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043704413,0.0003189809,0.0002756949,0.002308022,0.0015342063,0.0012410649,0.0007343107,0.00026488863,0.0012757544],"category_scores_gemma":[0.0015191257,0.00022991298,0.00020245291,0.004952369,0.000851596,0.00024790582,0.00064546254,0.00031378694,0.00019242665],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010637198,0.000016377377,0.9861333,0.000018028866,0.00006479757,0.000074127085,0.00079266255,0.00034786164,0.004033304,0.00014644238,0.00046592802,0.0078008324],"study_design_scores_gemma":[0.0000018109869,0.0000034867762,0.9986307,0.000006352596,0.000008310781,0.000014962617,0.00042097337,0.0002582202,0.00024045672,0.000014279947,0.0003941245,0.0000062114655],"about_ca_topic_score_codex":0.9867495,"about_ca_topic_score_gemma":0.99241954,"teacher_disagreement_score":0.01325053,"about_ca_system_score_codex":0.008547361,"about_ca_system_score_gemma":0.009544458,"threshold_uncertainty_score":0.062015772},"labels":[],"label_agreement":null},{"id":"W2186096621","doi":"10.1002/2015jb012467","title":"Multifrequential periodogram analysis of earthquake occurrence: An alternative approach to the Schuster spectrum, with two examples in central California","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; Ste. Anne's Hospital","funders":"U.S. Geological Survey; Southern California Earthquake Center; National Science Foundation","keywords":"Seismology; Geology; Periodogram; Series (stratigraphy); Fault (geology); Induced seismicity; Mathematics; Statistics; Paleontology","score_opus":0.08804173702369938,"score_gpt":0.3452226008246781,"score_spread":0.2571808638009787,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2186096621","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99236065,0.00023554999,0.0048031965,0.00007949194,0.000006730774,0.000015102617,0.0007565968,0.000089643996,0.0016529422],"genre_scores_gemma":[0.9954856,0.0000683151,0.0037525613,0.0000072806924,0.000007712285,0.000007061354,0.0004319044,0.000012532419,0.00022703526],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997919,0.000061063954,0.000015357868,0.00006359507,0.000047204532,0.000020892237],"domain_scores_gemma":[0.9991442,0.0003885724,0.00012654682,0.00009440743,0.00018721235,0.000059134236],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007664749,0.00023762643,0.00018890927,0.0024105085,0.0003063313,0.00059814204,0.00038899266,0.00025928256,0.00078680064],"category_scores_gemma":[0.001975776,0.000106841195,0.0002882638,0.0019320574,0.00021070919,0.00035870261,0.00033889478,0.00021723413,0.000066712644],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033621665,0.00015458687,0.8173456,0.00012614318,0.0002151889,0.0008062526,0.00092082383,0.06541486,0.005685342,0.004761484,0.0030209385,0.101212464],"study_design_scores_gemma":[0.000021731255,0.00005273552,0.75877047,0.000015494576,0.000032669865,0.00014063556,0.00037509462,0.2373806,0.0004327833,0.0014039662,0.0013391764,0.000034643424],"about_ca_topic_score_codex":0.116228834,"about_ca_topic_score_gemma":0.12363223,"teacher_disagreement_score":0.116228834,"about_ca_system_score_codex":0.00069054804,"about_ca_system_score_gemma":0.0004425626,"threshold_uncertainty_score":0.23110461},"labels":[],"label_agreement":null},{"id":"W2211577158","doi":"10.1002/2015jb012338","title":"Downdip variations in seismic reflection character: Implications for fault structure and seismogenic behavior in the Alaska subduction zone","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":73,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Seismology; Subduction; Trench; Transition zone; Reflection (computer programming); Wedge (geometry); Induced seismicity; Fault (geology); Submarine pipeline; Geophysics; Tectonics; Geometry; Geotechnical engineering","score_opus":0.07882716764501506,"score_gpt":0.3629786511622943,"score_spread":0.2841514835172792,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2211577158","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991893,0.000050794355,0.0002580618,0.000009825144,8.562981e-7,0.0000013733714,0.00007575377,0.000009494128,0.00040445323],"genre_scores_gemma":[0.9997763,0.000020147774,0.00008607946,0.0000020282191,6.0161324e-7,7.7872517e-7,0.000052733158,0.0000017215752,0.000059588496],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990594,0.000017356593,0.0000147458395,0.000029930447,0.000015761487,0.000016207265],"domain_scores_gemma":[0.99968076,0.00007185783,0.000112663256,0.000043459087,0.00004888017,0.00004243463],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025626188,0.00022283728,0.0001467784,0.00085020193,0.00018961921,0.00040382246,0.00019900771,0.00017758962,0.00116456],"category_scores_gemma":[0.0009185353,0.0001768957,0.00014126526,0.000501613,0.00024865175,0.00033292058,0.0003854008,0.0001564304,0.00016382594],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016116415,0.000028242048,0.94826883,0.00002879144,0.0000313037,0.00018479166,0.0005996269,0.0020590331,0.03898582,0.00007850912,0.000037713693,0.009536262],"study_design_scores_gemma":[0.0000011237229,0.000014812992,0.9976593,0.0000031863374,0.0000055611795,0.0000378699,0.00025452487,0.0013367699,0.00060067617,0.000030983472,0.000052285937,0.0000028621096],"about_ca_topic_score_codex":0.009818973,"about_ca_topic_score_gemma":0.009759523,"teacher_disagreement_score":0.009818973,"about_ca_system_score_codex":0.0002459902,"about_ca_system_score_gemma":0.00010848379,"threshold_uncertainty_score":0.01952362},"labels":[],"label_agreement":null},{"id":"W2280208863","doi":"10.1002/2015jb012453","title":"Rayleigh wave azimuthally anisotropic phase velocity maps beneath western Canada","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta; University of Calgary","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Craton; Lithosphere; Laurentia; Foreland basin; Asthenosphere; Seismic anisotropy; Geophysics; Anisotropy; Paleontology; Crust; Seismology; Mantle (geology); Tectonics; Physics","score_opus":0.04092351643871263,"score_gpt":0.3051730938125086,"score_spread":0.264249577373796,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2280208863","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99187547,0.00018235308,0.00014899966,0.0000405747,0.000003431988,0.0000069057255,0.0019005015,0.000045886398,0.005795904],"genre_scores_gemma":[0.9975712,0.00009922765,0.0002590265,0.0000068516847,0.0000015101461,0.0000028238305,0.00072137004,0.000004463888,0.0013335367],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993515,0.0000014551562,0.0000022403876,0.000012548459,0.000018599674,0.000030010495],"domain_scores_gemma":[0.999821,0.0000073892747,0.00002041147,0.0000041280523,0.000111820096,0.000035335393],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000044235065,0.00027063317,0.00010563205,0.001692267,0.0006323234,0.0005806069,0.00020669625,0.00010149018,0.0024956332],"category_scores_gemma":[0.00021670868,0.00008811719,0.00010336812,0.0013372353,0.00015973682,0.00012579239,0.0002789414,0.00010449336,0.00023982837],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003606689,0.000031237843,0.84976953,0.00009462077,0.00007022431,0.00072730356,0.0014000197,0.0045665973,0.060085207,0.00085348595,0.002910724,0.07913036],"study_design_scores_gemma":[0.000004257722,0.000005511647,0.9938671,0.000011404486,0.000008876141,0.00006362586,0.00044421124,0.0023597404,0.0013500499,0.0000318307,0.0018422811,0.000011112554],"about_ca_topic_score_codex":0.9402012,"about_ca_topic_score_gemma":0.96596485,"teacher_disagreement_score":0.059798777,"about_ca_system_score_codex":0.0035472955,"about_ca_system_score_gemma":0.0031995284,"threshold_uncertainty_score":0.12030184},"labels":[],"label_agreement":null},{"id":"W2288496799","doi":"10.1002/2015jb012416","title":"Seismic reflection imaging of the Juan de Fuca plate from ridge to trench: New constraints on the distribution of faulting and evolution of the crust prior to subduction","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":93,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Science Foundation","keywords":"Geology; Subduction; Seismology; Crust; Oceanic crust; Ridge; Trench; Receiver function; Transect; Fault (geology); Mantle (geology); Convergent boundary; Lithosphere; Paleontology; Tectonics","score_opus":0.04239652242047027,"score_gpt":0.31196079399586396,"score_spread":0.2695642715753937,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2288496799","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99823606,0.000045497483,0.00012489938,0.000010894867,0.0000017618488,0.0000019650217,0.00016240777,0.000014295775,0.001402143],"genre_scores_gemma":[0.9990508,0.00004692344,0.00037659824,0.0000049873656,0.0000025600875,0.000002169149,0.00022505902,0.0000041231024,0.00028674933],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995756,0.0000019997765,0.000002087326,0.000014910329,0.00001179494,0.000011635733],"domain_scores_gemma":[0.999915,0.000009349203,0.0000238603,0.000008857449,0.000025072623,0.00001792321],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010156977,0.00023001208,0.00013902149,0.00067476806,0.0002354454,0.00039228235,0.00017828966,0.0002361984,0.000992904],"category_scores_gemma":[0.000248601,0.00017594326,0.00012402805,0.00044008723,0.00019525479,0.00014593366,0.00028108325,0.00016201074,0.00013915969],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020758653,0.000056810888,0.7941212,0.00006401885,0.00006252524,0.0003857872,0.0009789449,0.0014210797,0.18108372,0.000119247044,0.000255263,0.02124391],"study_design_scores_gemma":[0.0000026688988,0.000017774046,0.9972236,0.0000070192505,0.000008414599,0.00007636744,0.0002036704,0.00075918855,0.0012787969,0.0000131269,0.0004051868,0.0000042746856],"about_ca_topic_score_codex":0.03061105,"about_ca_topic_score_gemma":0.08285459,"teacher_disagreement_score":0.03061105,"about_ca_system_score_codex":0.00032688328,"about_ca_system_score_gemma":0.0002943697,"threshold_uncertainty_score":0.0608657},"labels":[],"label_agreement":null},{"id":"W2296943930","doi":"10.1002/2015jb012603","title":"Discriminating induced seismicity from natural earthquakes using moment tensors and source spectra","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":120,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University; University of Calgary","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; Microseismic Industry Consortium","keywords":"Seismology; Geology; Intraplate earthquake; Moment tensor; Induced seismicity; Focal mechanism; Spurious relationship; Seismic moment; Spectral line; Tectonics; Moment magnitude scale; Magnitude (astronomy); Shield; Geometry; Physics; Fault (geology); Scaling; Petrology; Mathematics","score_opus":0.06606367543509702,"score_gpt":0.32284499486352974,"score_spread":0.25678131942843274,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2296943930","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9905054,0.00004176636,0.007613732,0.000023118606,0.000002756062,0.000014378865,0.00039650145,0.00011445418,0.0012879216],"genre_scores_gemma":[0.99664056,0.00003789937,0.002675846,0.0000029920843,0.0000015121931,0.0000031402083,0.00044316973,0.00001018107,0.00018469016],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990356,0.000007429683,0.0000064704045,0.000011683717,0.000052986343,0.000017812163],"domain_scores_gemma":[0.99964094,0.000094315204,0.00008483509,0.000028114186,0.00010811395,0.000043630855],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018563081,0.00030368307,0.0001107262,0.0011929146,0.00016748434,0.00039458598,0.00027753357,0.000166965,0.0009931499],"category_scores_gemma":[0.0016342867,0.00012304784,0.0001707433,0.0007908458,0.00020629242,0.00030156624,0.0002187339,0.00013196495,0.00013563792],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000268654,0.00013495065,0.72416955,0.00016089308,0.0001536899,0.00063337776,0.00040487666,0.08070235,0.08561857,0.0022090364,0.00091463176,0.10462937],"study_design_scores_gemma":[0.00001180749,0.00003868534,0.8915743,0.00000773988,0.000020865613,0.0001254291,0.00013059416,0.10019598,0.0068316483,0.00036345277,0.0006808185,0.000018575578],"about_ca_topic_score_codex":0.08397382,"about_ca_topic_score_gemma":0.21628913,"teacher_disagreement_score":0.08397382,"about_ca_system_score_codex":0.00069123646,"about_ca_system_score_gemma":0.00086560444,"threshold_uncertainty_score":0.16697007},"labels":[],"label_agreement":null},{"id":"W2316341725","doi":"10.1002/2015jb012415","title":"In situ stress magnitudes at the toe of the Nankai Trough Accretionary Prism, offshore Shikoku Island, Japan","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"","keywords":"Geology; Accretionary wedge; Thrust fault; Seafloor spreading; Seismology; Submarine pipeline; Thrust; Borehole; Differential stress; Slip (aerodynamics); Fault (geology); Tectonics; Subduction; Deformation (meteorology); Geotechnical engineering; Geophysics","score_opus":0.03230259012813515,"score_gpt":0.30356646764587303,"score_spread":0.2712638775177379,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2316341725","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992532,0.000019761439,0.00009221525,0.0000060876973,0.0000015258075,0.0000021413814,0.00019620423,0.000008121587,0.00042071388],"genre_scores_gemma":[0.9993206,0.000025747238,0.00024610973,0.000005391883,0.0000018475197,0.0000048942843,0.00024066461,0.0000017986703,0.0001528659],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998927,0.0000069155813,0.000011593154,0.00003817037,0.000028677357,0.000021938806],"domain_scores_gemma":[0.9997961,0.000014605348,0.00005064854,0.000013552178,0.000074545365,0.000050654337],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018322135,0.00040852712,0.00024358444,0.00069154386,0.00044525426,0.00038573434,0.00036701828,0.00032757837,0.0007262235],"category_scores_gemma":[0.00030248245,0.00025470147,0.0002134874,0.0006689883,0.0002610004,0.00030366136,0.00045351114,0.00017431332,0.00016541223],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014270855,0.000041505133,0.9467248,0.00006654589,0.00007659618,0.00032505367,0.0006275169,0.0022072536,0.041486274,0.000037923714,0.00013977518,0.008124022],"study_design_scores_gemma":[0.000007650701,0.000031015643,0.9960984,0.000005749466,0.000018647714,0.00003510607,0.00035749024,0.0020775027,0.0012230637,0.000009095349,0.00013044807,0.0000057105362],"about_ca_topic_score_codex":0.047377095,"about_ca_topic_score_gemma":0.12666126,"teacher_disagreement_score":0.047377095,"about_ca_system_score_codex":0.00041499405,"about_ca_system_score_gemma":0.00047710608,"threshold_uncertainty_score":0.0942027},"labels":[],"label_agreement":null},{"id":"W2321651621","doi":"10.1002/2015jb012778","title":"New insights into Phanerozoic tectonics of south China: Part 1, polyphase deformation in the Jiuling and Lianyunshan domains of the central Jiangnan Orogen","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":153,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Chinese Academy of Geological Sciences; China Institute of Atomic Energy; Chinese Academy of Sciences; National Natural Science Foundation of China","keywords":"Geology; Paleontology; Subduction; Phanerozoic; Seismology; Shear zone; Sinistral and dextral; Cretaceous; Lithosphere; Fibrous joint; Proterozoic; Tectonics; Structural basin; Cenozoic","score_opus":0.020083163422838314,"score_gpt":0.2628847255616504,"score_spread":0.24280156213881207,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2321651621","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977297,0.00045206727,0.00023988652,0.00004363886,0.0000023023324,0.0000058929318,0.00008942805,0.0000047594017,0.0014324168],"genre_scores_gemma":[0.99895716,0.00033156888,0.00019268552,0.000012593045,0.000003979756,0.0000041142634,0.00011497836,0.0000036622064,0.00037927195],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994075,0.00000546687,0.000006378406,0.000021053307,0.000013994611,0.000012316129],"domain_scores_gemma":[0.99990714,0.000010019673,0.000029960325,0.000010646486,0.000024051378,0.00001818798],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020921517,0.0002903363,0.00023465387,0.0019600284,0.0005008603,0.00047030812,0.00018717711,0.00020660638,0.0015618408],"category_scores_gemma":[0.00020112474,0.00018167707,0.00024170568,0.00235488,0.0006137611,0.0004801672,0.00047230642,0.00016010829,0.00009762152],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000093031806,0.000027674052,0.8611458,0.00024921828,0.00011082497,0.0008231788,0.006100055,0.0014653101,0.08232003,0.001319298,0.00018609919,0.04615945],"study_design_scores_gemma":[0.0000011474979,0.0000064734504,0.99850607,0.000004944365,0.0000071662075,0.000043478325,0.00038207823,0.00033352352,0.00018321285,0.00010253128,0.00042694306,0.0000024031597],"about_ca_topic_score_codex":0.044447165,"about_ca_topic_score_gemma":0.1108942,"teacher_disagreement_score":0.044447165,"about_ca_system_score_codex":0.00081339834,"about_ca_system_score_gemma":0.00075372553,"threshold_uncertainty_score":0.08837688},"labels":[],"label_agreement":null},{"id":"W2325344118","doi":"10.1002/2015jb012136","title":"Laboratory observations of time‐dependent frictional strengthening and stress relaxation in natural and synthetic fault gouges","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":132,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"National Science Foundation","keywords":"Shearing (physics); Geology; Creep; Calcite; Slip (aerodynamics); Feldspar; Shear (geology); Quartz; Fault gouge; Geotechnical engineering; Fault (geology); Mineralogy; Seismology; Petrology; Materials science; Composite material","score_opus":0.027909595858677392,"score_gpt":0.2842998314084204,"score_spread":0.256390235549743,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2325344118","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99978465,0.000012894067,0.000109893575,0.0000013990699,3.707608e-7,0.0000022267259,0.000036850724,0.000003957638,0.00004783838],"genre_scores_gemma":[0.9996215,0.000012594559,0.0001971797,0.0000026219554,5.359478e-7,0.0000058750775,0.000100666235,0.0000014619902,0.000057633202],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999317,0.000010546903,0.0000064820492,0.000018246543,0.00001666864,0.00001641413],"domain_scores_gemma":[0.99979943,0.000030041698,0.00007776218,0.000021607662,0.00003626507,0.00003501368],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012196622,0.00017931037,0.000118021446,0.00027598784,0.00017934934,0.00015820071,0.00015340872,0.00014362288,0.0003864707],"category_scores_gemma":[0.00023044233,0.00009901695,0.00012657266,0.00015637431,0.00038422065,0.00012182976,0.00020616953,0.00015158732,0.00005143025],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000119993114,0.000027629912,0.017466608,0.000016854106,0.000010179571,0.000052767555,0.00009564733,0.00016498537,0.98138154,0.000018761597,0.00001317847,0.00063190935],"study_design_scores_gemma":[0.000031505555,0.0019625972,0.46301937,0.0000068016857,0.000032187112,0.00038170887,0.00039733973,0.0023819217,0.5312481,0.00005552987,0.00046541588,0.000017517745],"about_ca_topic_score_codex":0.0019254365,"about_ca_topic_score_gemma":0.0032352635,"teacher_disagreement_score":0.0019254365,"about_ca_system_score_codex":0.00018490071,"about_ca_system_score_gemma":0.0000900388,"threshold_uncertainty_score":0.0038284063},"labels":[],"label_agreement":null},{"id":"W2326489194","doi":"10.1002/2015jb012460","title":"Structure and anisotropy of the crust in the Cyclades, Greece, using receiver functions constrained by in situ rock textural data","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Receiver function; Crust; CYCLADES; Anisotropy; Seismic anisotropy; Blueschist; Seismology; Petrology; Lithology; Magmatism; Subduction; Eclogite; Geophysics; Geochemistry; Mantle (geology); Tectonics","score_opus":0.049228167592121834,"score_gpt":0.31382110815581676,"score_spread":0.2645929405636949,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2326489194","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99903023,0.000027295036,0.00053306244,0.0000105205345,9.0025736e-7,0.0000024639346,0.0001225655,0.000021174419,0.0002517357],"genre_scores_gemma":[0.99910223,0.000026219472,0.00048396888,0.0000021431576,0.0000016091637,0.0000022013,0.00030280178,0.000006174517,0.00007267908],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998919,0.000020856161,0.0000073658757,0.00005359824,0.000011062911,0.000015212707],"domain_scores_gemma":[0.99978596,0.000060381888,0.00006133656,0.00003994628,0.000027713262,0.000024634539],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025293467,0.0006246486,0.0002238187,0.0011774354,0.00014690119,0.0006326522,0.0003622197,0.00044291755,0.00042239373],"category_scores_gemma":[0.00076071155,0.00027984363,0.00038066957,0.0007103159,0.0002829374,0.00038282946,0.00037677077,0.00019002048,0.00013594427],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004455758,0.00022378968,0.5398875,0.00013483797,0.0005191294,0.0009964261,0.0005235536,0.32162723,0.100015774,0.0006042143,0.00032886516,0.03469304],"study_design_scores_gemma":[0.00005486602,0.00008720626,0.62814236,0.00002731664,0.000103090344,0.0001618182,0.00029062957,0.3648696,0.0052757673,0.00034525857,0.00059334986,0.000048809692],"about_ca_topic_score_codex":0.022072539,"about_ca_topic_score_gemma":0.022745399,"teacher_disagreement_score":0.022072539,"about_ca_system_score_codex":0.00037108286,"about_ca_system_score_gemma":0.00038360906,"threshold_uncertainty_score":0.04388815},"labels":[],"label_agreement":null},{"id":"W2337689892","doi":"10.1002/2015jb012577","title":"A paleomagnetic and rock magnetic study of the Manicouagan impact structure: Implications for crater formation and geodynamo effects","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of New Brunswick","funders":"Canadian Space Agency; Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; Natural Resources Canada; Deutsche Forschungsgemeinschaft","keywords":"Geology; Impact crater; Paleomagnetism; Remanence; Demagnetizing field; Impact structure; Geophysics; Rock magnetism; Natural remanent magnetization; Magnetic anomaly; Magnetic mineralogy; Pyrrhotite; Meteorite; Petrology; Mineralogy; Geochemistry; Magnetization; Magnetic field; Astrobiology; Pyrite","score_opus":0.01983808461182699,"score_gpt":0.3201827122052098,"score_spread":0.30034462759338276,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2337689892","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967158,0.00016380692,0.00005711273,0.000028142249,0.000001920038,0.000009179542,0.00023742816,0.00000548066,0.0027812088],"genre_scores_gemma":[0.99877113,0.00011485318,0.00015171626,0.000008434667,0.0000021569172,0.0000055513447,0.0002544074,0.0000034690627,0.000688276],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992156,0.000004030521,0.0000022330453,0.000018934707,0.000023273768,0.000029970133],"domain_scores_gemma":[0.9998605,0.000008970912,0.000025636498,0.000007983977,0.00007285351,0.000024059938],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010564424,0.00026258585,0.00022676947,0.0013626355,0.0011052118,0.0005768338,0.00033318857,0.00019047034,0.0015076315],"category_scores_gemma":[0.00032117587,0.00020379738,0.0001711025,0.0015475132,0.00055223645,0.00015308404,0.0004412199,0.00017657805,0.00017193446],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025036428,0.00002071757,0.9573764,0.000059985858,0.00005818488,0.0003995542,0.0011127158,0.00076113164,0.027400883,0.00021516944,0.00028094338,0.012063905],"study_design_scores_gemma":[0.0000022768966,0.0000105461095,0.9983444,0.0000059431723,0.0000062280938,0.00008304276,0.00024264891,0.00016131223,0.00048516685,0.000008293484,0.0006475224,0.0000025271106],"about_ca_topic_score_codex":0.7356759,"about_ca_topic_score_gemma":0.8993754,"teacher_disagreement_score":0.26432413,"about_ca_system_score_codex":0.0039108763,"about_ca_system_score_gemma":0.0024273042,"threshold_uncertainty_score":0.5317615},"labels":[],"label_agreement":null},{"id":"W2339024901","doi":"10.1002/2015jb012627","title":"Submarine groundwater discharge as a possible formation mechanism for permafrost‐associated gas hydrate on the circum‐Arctic continental shelf","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Department of Energy","keywords":"Permafrost; Clathrate hydrate; Geology; Methane; Arctic; Continental shelf; Submarine groundwater discharge; Hydrate; Submarine pipeline; Continental margin; Groundwater; Oceanography; Aquifer; Geotechnical engineering; Tectonics; Paleontology","score_opus":0.02712175018924683,"score_gpt":0.2904480425818722,"score_spread":0.26332629239262534,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2339024901","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983341,0.000042111045,0.00068059226,0.00006483532,0.0000036087793,0.000005367182,0.000084704065,0.00002562066,0.0007591213],"genre_scores_gemma":[0.9995765,0.000018990535,0.00020119414,0.000004709717,0.0000010697443,0.0000021281528,0.00003757807,0.0000019149493,0.00015585526],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999572,0.0000073024826,0.0000020216141,0.000010306403,0.000007305324,0.000015940965],"domain_scores_gemma":[0.9999324,0.0000120266295,0.000014144329,0.0000054027837,0.000016967659,0.000019065994],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011767308,0.0003909004,0.00024224368,0.00028306068,0.00069126906,0.0006550052,0.00054996565,0.0005318254,0.0006426898],"category_scores_gemma":[0.00016673638,0.00023268817,0.0004936777,0.00016692998,0.00041031523,0.00030681674,0.00039281766,0.00020878096,0.00004888239],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002888662,0.00013672218,0.2392342,0.000058800393,0.00009524434,0.00054937624,0.00023774584,0.6764459,0.07132104,0.0053108837,0.0005193441,0.0058019604],"study_design_scores_gemma":[0.000045476023,0.00010123889,0.06460721,0.000008835692,0.000034035613,0.000039555154,0.00019253089,0.9296382,0.0042052553,0.0005602656,0.00053521874,0.000032144162],"about_ca_topic_score_codex":0.29013056,"about_ca_topic_score_gemma":0.14660239,"teacher_disagreement_score":0.29013056,"about_ca_system_score_codex":0.0024394174,"about_ca_system_score_gemma":0.0016498961,"threshold_uncertainty_score":0.5768836},"labels":[],"label_agreement":null},{"id":"W2343093903","doi":"10.1002/2015jb012454","title":"Quantifying structural states of soft mudrocks","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Grouting, Rheology, and Soil Mechanics","field":"Engineering","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Mitacs; Carbon Management Canada; Imperial Oil Limited","keywords":"Homogenization (climate); Anisotropy; Compressibility; Oil shale; Geotechnical engineering; Permeability (electromagnetism); Geology; Mineralogy; Materials science; Composite material; Thermodynamics; Chemistry","score_opus":0.05061613810207333,"score_gpt":0.34589673298664886,"score_spread":0.29528059488457553,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2343093903","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8111218,0.000119325094,0.18688872,0.00002952287,0.0000036229949,0.00002856487,0.00011061404,0.00013851238,0.0015593272],"genre_scores_gemma":[0.99557614,0.000018558727,0.0042035906,0.0000050694557,8.117018e-7,0.000009307419,0.000040145995,0.000004497701,0.00014190175],"study_design_codex":"simulation_or_modeling","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99978346,0.000029598581,0.000013293461,0.00006984979,0.00006896856,0.000034806737],"domain_scores_gemma":[0.99961156,0.00012502233,0.00012389502,0.000045427412,0.00007157102,0.000022464106],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037722068,0.00041406165,0.00029322185,0.0013301482,0.00024434066,0.0005328783,0.00053055986,0.00039945616,0.00036741386],"category_scores_gemma":[0.0009977088,0.00023292856,0.00035134662,0.0004338128,0.000663037,0.0006416842,0.0006409819,0.00024467564,0.000061356644],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000095056916,0.0000384966,0.031643655,0.00006733343,0.000046397523,0.00014012295,0.00010302304,0.8969427,0.04338543,0.0054589696,0.00009798348,0.021980932],"study_design_scores_gemma":[0.000002941016,0.000022061366,0.010050058,0.000004664304,0.000010016066,0.000026416163,0.000034198554,0.98255676,0.0059066084,0.0012759765,0.00009746239,0.000012826612],"about_ca_topic_score_codex":0.0071926266,"about_ca_topic_score_gemma":0.0069273515,"teacher_disagreement_score":0.0071926266,"about_ca_system_score_codex":0.0006912908,"about_ca_system_score_gemma":0.00044227688,"threshold_uncertainty_score":0.014301479},"labels":[],"label_agreement":null},{"id":"W2344343959","doi":"10.1002/2015jb012579","title":"Effects of olivine fabric, melt‐rock reaction, and hydration on the seismic properties of peridotites: Insight from the Luobusha ophiolite in the Tibetan Plateau","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Bedford Institute of Oceanography; Polytechnique Montréal","funders":"National Natural Science Foundation of China","keywords":"Olivine; Geology; Pyroxene; Anisotropy; Mantle (geology); Mineralogy; Ophiolite; Peridotite; Seismic anisotropy; Plateau (mathematics); Dissolution; Geochemistry; Tectonics; Chemistry; Seismology","score_opus":0.028416449492756873,"score_gpt":0.255240203018413,"score_spread":0.22682375352565612,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2344343959","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997899,0.000020484234,0.000039359915,0.0000028169545,1.5641638e-7,7.776217e-7,0.000022186327,0.0000020616221,0.00012245486],"genre_scores_gemma":[0.9998604,0.000011459087,0.000039343664,0.00000201743,4.92621e-7,0.000001020021,0.000044723976,0.0000014681582,0.000039092294],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99995136,0.0000063389416,0.000004447489,0.000013120733,0.000012250927,0.000012437042],"domain_scores_gemma":[0.9998944,0.000022297658,0.000030583586,0.0000063798193,0.000021756865,0.000024539264],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017721106,0.00025341258,0.00016991273,0.0007140958,0.0002347859,0.00033865933,0.00017035124,0.00019376496,0.00071059586],"category_scores_gemma":[0.000202658,0.00015476013,0.00017770345,0.00038016096,0.00030957727,0.00017657029,0.00022137922,0.00013681922,0.0000749275],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032144063,0.000048340848,0.321435,0.000054362485,0.0000491921,0.00030699972,0.00039593986,0.0011932991,0.67114764,0.000052853437,0.000022458598,0.0049724234],"study_design_scores_gemma":[0.0000067405595,0.00005578693,0.9872731,0.00000255989,0.000012274061,0.00007186605,0.00025892354,0.00224273,0.009958483,0.000018559296,0.0000938539,0.0000051665997],"about_ca_topic_score_codex":0.0073197247,"about_ca_topic_score_gemma":0.009188358,"teacher_disagreement_score":0.0073197247,"about_ca_system_score_codex":0.0002596477,"about_ca_system_score_gemma":0.00014931538,"threshold_uncertainty_score":0.014554203},"labels":[],"label_agreement":null},{"id":"W2361820528","doi":"10.1002/2016jb012841","title":"A new back‐and‐forth iterative method for time‐reversed convection modeling: Implications for the Cenozoic evolution of 3‐D structure and dynamics of the mantle","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Université de Montréal","keywords":"Mantle convection; Mantle (geology); Geology; Buoyancy; Subduction; Hotspot (geology); Seismic tomography; Plate tectonics; Geophysics; Convection; Mantle plume; Tectonics; Seismology; Lithosphere; Mechanics; Physics","score_opus":0.028999999076375377,"score_gpt":0.32245101847555685,"score_spread":0.2934510193991815,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2361820528","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.031520974,0.00008199088,0.96636903,0.00024803512,0.00004061259,0.00010050947,0.00005718719,0.0004200676,0.0011616455],"genre_scores_gemma":[0.2547069,0.000087492095,0.741594,0.00013497799,0.000043883712,0.000459517,0.00015575005,0.00026636012,0.0025511018],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996711,0.00016036529,0.000022081616,0.000036674057,0.00008245032,0.000027316764],"domain_scores_gemma":[0.99898213,0.0006089208,0.000088266854,0.000059350055,0.00020627322,0.000055077548],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017071936,0.000667311,0.00068325526,0.00045885146,0.00054233667,0.00069430977,0.0015833005,0.0014837789,0.0015877072],"category_scores_gemma":[0.0031492454,0.0005144142,0.0006895159,0.00039179373,0.00072047854,0.0005726495,0.0011085733,0.0011212769,0.0003278261],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000050442202,0.00006211038,0.0009814037,0.000027426833,0.00003854716,0.000053874974,0.000052589385,0.9728538,0.0032555517,0.0043324144,0.00035728532,0.017934643],"study_design_scores_gemma":[0.0000027578253,0.0000029456903,0.000013528961,6.675987e-7,6.031177e-7,8.3056904e-7,0.0000011608547,0.9997037,0.00007385129,0.00013936569,0.000059301634,0.0000012734924],"about_ca_topic_score_codex":0.015041584,"about_ca_topic_score_gemma":0.013697793,"teacher_disagreement_score":0.015041584,"about_ca_system_score_codex":0.00062903785,"about_ca_system_score_gemma":0.0015823157,"threshold_uncertainty_score":0.029908061},"labels":[],"label_agreement":null},{"id":"W2392172767","doi":"10.1002/2015jb012641","title":"Constraints on the heterogeneity spectrum of Earth's upper mantle","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Coda; Mantle (geology); Scattering; Geology; Seismic tomography; Geophysics; Computational physics; Tomography; Wavelength; Physics; Seismology; Optics","score_opus":0.043706299969368,"score_gpt":0.31023317636011216,"score_spread":0.2665268763907442,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2392172767","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98564607,0.00011529501,0.011223848,0.00009175592,0.000003526288,0.00000384869,0.00024103129,0.000103943836,0.0025706226],"genre_scores_gemma":[0.9993388,0.000021606773,0.00046582983,0.000007063953,0.0000017566642,0.000001958277,0.00011069088,0.000008976593,0.000043421605],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999001,0.000019714053,0.0000060635684,0.000029635845,0.000019744139,0.000024683117],"domain_scores_gemma":[0.99932456,0.00031952496,0.00011423444,0.00011364593,0.00007336519,0.000054618577],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037294455,0.00033874813,0.00024962396,0.00062461785,0.00020606497,0.0007844047,0.0005191816,0.00039673323,0.0010252564],"category_scores_gemma":[0.0024496594,0.0002525828,0.00036821453,0.00035971776,0.00033689578,0.0011542548,0.0005965829,0.00034157824,0.00014205926],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016312544,0.000059196296,0.1415441,0.000050537994,0.00015456311,0.00023703596,0.00008142993,0.795638,0.040481683,0.010682424,0.00037401597,0.010533872],"study_design_scores_gemma":[0.000028035962,0.000022228118,0.08496466,0.000016453318,0.000026136127,0.000057013487,0.000066986446,0.89971113,0.0061065573,0.008323502,0.00065483805,0.000022452181],"about_ca_topic_score_codex":0.0058009946,"about_ca_topic_score_gemma":0.0035305223,"teacher_disagreement_score":0.0058009946,"about_ca_system_score_codex":0.00051899016,"about_ca_system_score_gemma":0.00025203385,"threshold_uncertainty_score":0.011534452},"labels":[],"label_agreement":null},{"id":"W2396544295","doi":"10.1002/2015jb012320","title":"Experimental verification of a prediction model for hydrate‐bearing sand","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Hydrate; Saturation (graph theory); Seeding; Clathrate hydrate; Geotechnical engineering; Experimental data; Water saturation; Geology; Materials science; Thermodynamics; Porosity; Mathematics; Chemistry; Statistics; Physics","score_opus":0.047206914783365285,"score_gpt":0.33501608520257964,"score_spread":0.28780917041921433,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2396544295","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9170375,0.000059217185,0.079641916,0.00006917877,0.00002348718,0.00012166046,0.00041875942,0.00080919504,0.0018189508],"genre_scores_gemma":[0.9939208,0.000019531928,0.005577889,0.0000039527795,0.0000011847125,0.000040743686,0.000085068874,0.000020584352,0.00033017137],"study_design_codex":"simulation_or_modeling","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9994704,0.000052274856,0.000032220567,0.00011160108,0.00029065125,0.000042953157],"domain_scores_gemma":[0.9989279,0.00046999016,0.0001014792,0.00019835438,0.0002766827,0.000025626756],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010140694,0.0005466502,0.00037249422,0.00027598024,0.00030098716,0.00033547962,0.0010497665,0.0005054672,0.0014267014],"category_scores_gemma":[0.001656067,0.0002590609,0.00030552744,0.000196574,0.00045861944,0.00038514275,0.00032553298,0.00034863583,0.00029836295],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00069546537,0.000347491,0.0095940465,0.00016788229,0.00003093903,0.00023829902,0.00019737905,0.49403915,0.4724847,0.0008812681,0.00038981557,0.02093357],"study_design_scores_gemma":[0.000028101034,0.00026456258,0.003421861,0.000004688108,0.000010219069,0.000026163809,0.000022915063,0.8384462,0.1573624,0.000066904526,0.0003305585,0.000015425258],"about_ca_topic_score_codex":0.008211864,"about_ca_topic_score_gemma":0.006053263,"teacher_disagreement_score":0.008211864,"about_ca_system_score_codex":0.000661928,"about_ca_system_score_gemma":0.0006657705,"threshold_uncertainty_score":0.016328096},"labels":[],"label_agreement":null},{"id":"W2410027256","doi":"10.1002/2015jb012348","title":"Three billion years of crustal evolution in eastern Canada: Constraints from receiver functions","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Environment Research Council; Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; Sight Research UK; Leverhulme Trust; National Science Foundation","keywords":"Geology; Mafic; Archean; Proterozoic; Crust; Mantle (geology); Shear zone; Craton; Massif; Crustal recycling; Petrology; Geochemistry; Underplating; Tectonics; Lithosphere; Seismology; Continental crust","score_opus":0.032371976738795535,"score_gpt":0.2578688311124898,"score_spread":0.22549685437369427,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2410027256","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9911499,0.0011073721,0.00039967414,0.00017009866,0.000004480849,0.000006134368,0.0034347705,0.000030575287,0.0036969301],"genre_scores_gemma":[0.99643046,0.0002423986,0.0002414225,0.000021291271,0.0000015248878,0.0000018983889,0.0016301506,0.000009141765,0.0014216711],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997547,0.0000120256855,0.000009321807,0.000052120206,0.00007420495,0.00009755833],"domain_scores_gemma":[0.9988003,0.00011334651,0.00015135939,0.00006183041,0.0007091695,0.00016407108],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036802507,0.00027241214,0.00025116236,0.001879971,0.0015049909,0.0014176652,0.0006606505,0.00035110288,0.0023908995],"category_scores_gemma":[0.0011747025,0.0002067254,0.00030259465,0.003206992,0.0006471546,0.00035585123,0.00059985736,0.0003149405,0.00028315245],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013257231,0.000018444456,0.95758486,0.00004990301,0.00018266772,0.00039360314,0.0011841384,0.0032514748,0.0043240213,0.0019277106,0.001415747,0.029534867],"study_design_scores_gemma":[0.000003229342,0.000006550769,0.992046,0.000025093492,0.000032531887,0.000079600984,0.0006383773,0.0023901588,0.00032890087,0.0001605168,0.0042718234,0.000017161941],"about_ca_topic_score_codex":0.9898784,"about_ca_topic_score_gemma":0.9941281,"teacher_disagreement_score":0.01294075,"about_ca_system_score_codex":0.01294075,"about_ca_system_score_gemma":0.00963813,"threshold_uncertainty_score":0.09389216},"labels":[],"label_agreement":null},{"id":"W2426019861","doi":"10.1002/2016jb012884","title":"Modeling 3‐D crustal velocities in the United States and Canada","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"National Oceanic and Atmospheric Administration","keywords":"Geology; Post-glacial rebound; Glacier; Geodetic datum; Geodesy; Residual; Glacial period; Longitude; Reference frame; Ice caps; Tectonics; Field (mathematics); Ice sheet; Latitude; Geophysics; Seismology; Geomorphology; Frame (networking)","score_opus":0.045821759876559696,"score_gpt":0.2947027526782399,"score_spread":0.24888099280168022,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2426019861","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95214504,0.0004202791,0.015935324,0.0005072537,0.000040636583,0.00010195879,0.0077093956,0.00049497234,0.022645142],"genre_scores_gemma":[0.98311156,0.00034685974,0.009917575,0.00005587951,0.0000032273276,0.000045386416,0.0029899683,0.000045312114,0.0034841895],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998783,0.00000961738,0.000005465434,0.00002815835,0.000046213416,0.000032133597],"domain_scores_gemma":[0.9996809,0.000037853744,0.00002696363,0.0000137547695,0.00019725933,0.00004335643],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023366483,0.0004421051,0.00021804219,0.0010821945,0.0015355818,0.0014166867,0.0011634356,0.0004938377,0.0012576215],"category_scores_gemma":[0.0009995741,0.0002785279,0.00056575675,0.0016043993,0.0005207902,0.0004448964,0.0006474439,0.0004708451,0.00018165004],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004836297,0.000035990113,0.052295227,0.000023120778,0.00007209458,0.000115597264,0.00017362692,0.9276447,0.0006045738,0.004353191,0.0025078251,0.012125646],"study_design_scores_gemma":[0.00001636696,0.000009124661,0.018011658,0.000020688392,0.000023727956,0.000019893385,0.0001711828,0.9745224,0.00045038507,0.0007695395,0.0059554735,0.000029441735],"about_ca_topic_score_codex":0.990812,"about_ca_topic_score_gemma":0.9839363,"teacher_disagreement_score":0.021974986,"about_ca_system_score_codex":0.021974986,"about_ca_system_score_gemma":0.015447808,"threshold_uncertainty_score":0.15944046},"labels":[],"label_agreement":null},{"id":"W2432779761","doi":"10.1002/2015jb012628","title":"Axial‐type olivine crystallographic preferred orientations: The effect of strain geometry on mantle texture","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Boston College; National Science Foundation","keywords":"Olivine; Geology; Seismic anisotropy; Mantle (geology); Peridotite; Electron backscatter diffraction; Anisotropy; Mineralogy; Deformation mechanism; Mantle wedge; Xenolith; Geometry; Geophysics; Subduction; Crystallography; Seismology; Microstructure; Physics; Tectonics; Chemistry; Optics","score_opus":0.025470888965173875,"score_gpt":0.31569457962657377,"score_spread":0.2902236906613999,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2432779761","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992144,0.000066331035,0.00023634634,0.000003972915,5.410292e-7,0.0000014902708,0.00010292352,0.000006717712,0.00036717765],"genre_scores_gemma":[0.99978644,0.000018426776,0.000074511954,0.0000015422164,3.602781e-7,8.774857e-7,0.00005664615,0.0000046059117,0.000056558267],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99986696,0.000016585933,0.000008259229,0.00003558796,0.000039257568,0.000033387827],"domain_scores_gemma":[0.99968135,0.00008503917,0.00009358708,0.000053992357,0.00005406176,0.00003203435],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001453939,0.00022774648,0.00016114858,0.000552757,0.00018585504,0.0005991143,0.00022186081,0.0001642791,0.0009014463],"category_scores_gemma":[0.0005660413,0.00017853956,0.00013848326,0.00034516337,0.00060046226,0.00020792928,0.00026907402,0.00013050783,0.00012503026],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029066388,0.000016044705,0.16515742,0.00006526152,0.00006287654,0.0001246708,0.00016903531,0.0018348829,0.82647306,0.00015765277,0.00004753096,0.005600997],"study_design_scores_gemma":[0.0000039936094,0.00004565569,0.9320081,0.0000046771315,0.000025535604,0.00015634116,0.00016721307,0.0029544276,0.064281374,0.000080460886,0.00026033077,0.000011908727],"about_ca_topic_score_codex":0.0047255447,"about_ca_topic_score_gemma":0.0055007692,"teacher_disagreement_score":0.0047255447,"about_ca_system_score_codex":0.00024242784,"about_ca_system_score_gemma":0.00013909282,"threshold_uncertainty_score":0.009396076},"labels":[],"label_agreement":null},{"id":"W2433263593","doi":"10.1002/2016jb012838","title":"Subduction beneath Laurentia modified the eastern North American cratonic edge: Evidence from <i>P</i> wave and <i>S</i> wave tomography","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Environment Research Council; Sight Research UK; Leverhulme Trust","keywords":"Geology; Archean; Proterozoic; Craton; Subduction; Laurentia; Lithosphere; Mantle (geology); Paleontology; Plate tectonics; Tectonics; Seismology; Earth science; Geophysics","score_opus":0.04862935299519951,"score_gpt":0.28404062132189284,"score_spread":0.23541126832669335,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2433263593","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978957,0.00004873178,0.000105392435,0.000038193044,0.0000011252612,0.000003957106,0.00023243402,0.000014445505,0.0016601183],"genre_scores_gemma":[0.9994804,0.00004873215,0.0001241876,0.000010188409,9.358503e-7,0.0000018282234,0.00013935051,0.0000033436768,0.00019095009],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992335,0.00000452335,0.0000036141103,0.000023849921,0.000020721685,0.00002397345],"domain_scores_gemma":[0.9997205,0.000028799743,0.00007992372,0.000025799876,0.00011079919,0.00003411636],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012976724,0.00022357215,0.00013177909,0.0008004599,0.0006044688,0.0009170238,0.00042036458,0.0003433275,0.0010436181],"category_scores_gemma":[0.00043130698,0.00021705213,0.00012655022,0.0009484703,0.0006034071,0.00030643205,0.00047988945,0.00026652106,0.00015282734],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011731826,0.000037349735,0.96104795,0.000026572236,0.00006526146,0.0004908458,0.00094336993,0.0016967991,0.02231874,0.0002590055,0.00036209341,0.012634687],"study_design_scores_gemma":[0.0000043361647,0.0000056973836,0.996527,0.00000940758,0.000014504544,0.000051419935,0.0004485975,0.0018314526,0.000674398,0.0000256301,0.0004012389,0.000006279129],"about_ca_topic_score_codex":0.52590775,"about_ca_topic_score_gemma":0.7260123,"teacher_disagreement_score":0.47409225,"about_ca_system_score_codex":0.0013240296,"about_ca_system_score_gemma":0.0011940098,"threshold_uncertainty_score":0.95376855},"labels":[],"label_agreement":null},{"id":"W2465105491","doi":"10.1002/2016jb013184","title":"The role of crystallization‐driven exsolution on the sulfur mass balance in volcanic arc magmas","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; U.S. Geological Survey; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; National Science Foundation","keywords":"Sulfur; Sulfate aerosol; Geology; Volcano; Sulfide; Chemistry; Earth science; Geochemistry; Atmospheric sciences; Stratosphere","score_opus":0.021506972995816945,"score_gpt":0.26082949603547356,"score_spread":0.23932252303965662,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2465105491","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971221,0.00063303876,0.0006209113,0.00014467776,0.000006366483,0.000004310807,0.00009185191,0.00003662998,0.0013401469],"genre_scores_gemma":[0.9996575,0.00010055194,0.00007862265,0.000005438597,0.0000054598413,9.350455e-7,0.000029542121,0.0000055823707,0.00011626557],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99990845,0.000012151406,0.0000076242836,0.000029141422,0.000021445263,0.000021196127],"domain_scores_gemma":[0.99983823,0.000050092764,0.000033697856,0.0000133859285,0.000035286368,0.000029201887],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002864892,0.0003189566,0.00024081799,0.0006777579,0.00034498767,0.00069643237,0.00033959304,0.0003729979,0.0012228674],"category_scores_gemma":[0.0004143987,0.00018935904,0.00017562664,0.00019594411,0.00058536447,0.0007108952,0.0004703859,0.00021522628,0.00018322484],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009713362,0.00009911192,0.20107056,0.00022499492,0.00017676127,0.00065397966,0.00040592276,0.015767729,0.7526346,0.00496111,0.00021827374,0.02281566],"study_design_scores_gemma":[0.000075571916,0.000369509,0.6083841,0.000023908417,0.00010095931,0.00041397635,0.0005590088,0.16108343,0.21803214,0.00772818,0.0031773285,0.000051946703],"about_ca_topic_score_codex":0.0060607237,"about_ca_topic_score_gemma":0.0029684475,"teacher_disagreement_score":0.0060607237,"about_ca_system_score_codex":0.00089396467,"about_ca_system_score_gemma":0.00027901988,"threshold_uncertainty_score":0.012050867},"labels":[],"label_agreement":null},{"id":"W2476463576","doi":"10.1002/2016jb013102","title":"Fluid‐assisted deformation of the subduction interface: Coupled and decoupled regimes from 2‐D hydromechanical modeling","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"European Commission","keywords":"Subduction; Geology; Slab; Cohesion (chemistry); Shear (geology); Mechanics; Deformation (meteorology); Geophysics; Petrology; Tectonics; Seismology; Physics","score_opus":0.04695211259650907,"score_gpt":0.30594772046114466,"score_spread":0.2589956078646356,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2476463576","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.87737435,0.00045126822,0.10715157,0.0004841475,0.000049307557,0.00013226974,0.00053113984,0.00033230986,0.013493771],"genre_scores_gemma":[0.99288964,0.00015026121,0.0057355496,0.000041077798,0.000015590407,0.000076630655,0.0001173049,0.00002944078,0.00094437046],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99988604,0.000033107404,0.000008005042,0.000023870762,0.000029599558,0.000019402423],"domain_scores_gemma":[0.99976164,0.00010809813,0.000046039248,0.000025804702,0.00003344415,0.000025023919],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021494982,0.00065094646,0.0005856117,0.0005891524,0.00036942985,0.0009706066,0.0009786573,0.0013945365,0.0012441949],"category_scores_gemma":[0.0008517758,0.00050378195,0.0008040809,0.0004255015,0.00083455845,0.00078577903,0.0009104394,0.0006359081,0.00013884979],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017746168,0.000030426272,0.0012857795,0.000020366388,0.000015171112,0.000051454066,0.000035169694,0.99367404,0.0026058014,0.0013079502,0.000063599786,0.0008925338],"study_design_scores_gemma":[0.0000026959156,0.0000023726977,0.00020231068,0.0000010144792,0.0000010284461,0.0000019514005,0.000002351821,0.9995432,0.00007001992,0.00013758155,0.00003342409,0.000002073083],"about_ca_topic_score_codex":0.012698885,"about_ca_topic_score_gemma":0.006743389,"teacher_disagreement_score":0.012698885,"about_ca_system_score_codex":0.0007657913,"about_ca_system_score_gemma":0.0006532659,"threshold_uncertainty_score":0.025249958},"labels":[],"label_agreement":null},{"id":"W2477550485","doi":"10.1002/2016jb012857","title":"Spatiotemporal evolution of slow slip events in a nonplanar fault model for northern Cascadia subduction zone","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":75,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; McGill University","keywords":"Geology; Slip (aerodynamics); Subduction; Episodic tremor and slip; Seismology; Fault (geology); Tectonics; Physics","score_opus":0.046797554330904156,"score_gpt":0.3135177467491904,"score_spread":0.26672019241828626,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2477550485","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99617505,0.00007505866,0.0018144192,0.00011643243,0.000010350042,0.00001006837,0.000306184,0.00006713313,0.0014252483],"genre_scores_gemma":[0.9989686,0.000036848818,0.00025326412,0.000007123394,0.000002541497,0.000010023834,0.00017919802,0.000008056121,0.0005342946],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999232,0.000017047547,0.0000048871025,0.00002304541,0.000008918482,0.000022830072],"domain_scores_gemma":[0.99976975,0.00006393541,0.00004343039,0.00002347201,0.000036007597,0.000063508385],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019200219,0.00062256836,0.00048525597,0.00066077954,0.0005043667,0.0007533335,0.0012220482,0.0011656166,0.0022839308],"category_scores_gemma":[0.0006837959,0.00030218615,0.0007222931,0.00041863305,0.00067870674,0.00027884703,0.0005220469,0.00050902937,0.00014068294],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000044711127,0.000034549095,0.011367041,0.000011926793,0.00002771545,0.00015888477,0.000029038092,0.9864807,0.00085919985,0.00043369064,0.00013314789,0.00041934356],"study_design_scores_gemma":[0.000012261436,0.000015820393,0.003599986,0.0000022628096,0.000009029399,0.000009617459,0.000022025355,0.9960634,0.00007013368,0.000112121845,0.000078028,0.0000053951167],"about_ca_topic_score_codex":0.1343171,"about_ca_topic_score_gemma":0.05793457,"teacher_disagreement_score":0.1343171,"about_ca_system_score_codex":0.0016766199,"about_ca_system_score_gemma":0.0008120411,"threshold_uncertainty_score":0.2670706},"labels":[],"label_agreement":null},{"id":"W2496989734","doi":"10.1002/2016jb013228","title":"A 2‐D tomographic model of the Juan de Fuca plate from accretion at axial seamount to subduction at the Cascadia margin from an active source ocean bottom seismometer survey","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Woods Hole Oceanographic Institution; National Science Foundation","keywords":"Geology; Subduction; Seismology; Crust; Oceanic crust; Mantle (geology); Seamount; Seafloor spreading; Seismic tomography; Detachment fault; Underplating; Geophysics; Petrology; Tectonics; Paleontology","score_opus":0.04900055408168715,"score_gpt":0.3017570488467472,"score_spread":0.25275649476506007,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2496989734","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.993331,0.00004416412,0.0018361573,0.00013707664,0.0000068207532,0.000019773448,0.0009989776,0.0002455874,0.0033802586],"genre_scores_gemma":[0.9979511,0.000038630507,0.00088741817,0.0000095179785,0.000003000594,0.000014050156,0.00046197156,0.000016347316,0.00061799056],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999552,0.000006400367,0.0000024237886,0.000017199769,0.000008185477,0.000010592299],"domain_scores_gemma":[0.99991477,0.000016134587,0.000013682554,0.000013576374,0.000016984148,0.000024920908],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011756027,0.00052339217,0.00022693428,0.0006970868,0.0005074106,0.00076261,0.00087403244,0.0009177606,0.0029797237],"category_scores_gemma":[0.00031871037,0.0004906899,0.00071436935,0.0007009118,0.00047376877,0.0002512213,0.00040962957,0.000308631,0.00028384113],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015874843,0.00007104377,0.054293375,0.000032229378,0.00009018073,0.00042160237,0.00016555452,0.93401676,0.006571562,0.00067196303,0.0004409931,0.0030658976],"study_design_scores_gemma":[0.00006640388,0.000052763564,0.06678569,0.000011730957,0.000035056186,0.00007589857,0.00014238748,0.93151236,0.00043824204,0.00032748756,0.00052628154,0.000025639192],"about_ca_topic_score_codex":0.16556399,"about_ca_topic_score_gemma":0.11299958,"teacher_disagreement_score":0.16556399,"about_ca_system_score_codex":0.0017713322,"about_ca_system_score_gemma":0.0012876991,"threshold_uncertainty_score":0.32920063},"labels":[],"label_agreement":null},{"id":"W2507701880","doi":"10.1002/2015jb012311","title":"The damage is done: Low fault friction recorded in the damage zone of the shallow Japan Trench décollement","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Science Foundation","keywords":"Geology; Trench; Slip (aerodynamics); Seismology; Décollement; Cataclastic rock; Fault (geology); Strike-slip tectonics; Drilling; Shear zone; Shear (geology); Petrology; Materials science; Composite material; Tectonics","score_opus":0.03637898421134305,"score_gpt":0.30821931956362264,"score_spread":0.2718403353522796,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2507701880","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997321,0.000017682722,0.00004892764,0.0000020382045,3.4077118e-7,0.0000010566182,0.00006811827,0.0000036911479,0.00012603517],"genre_scores_gemma":[0.9997955,0.00000855372,0.000049605023,0.0000012559989,3.4870482e-7,9.665714e-7,0.00006429317,8.9482114e-7,0.00007853128],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999323,0.0000025432307,0.0000039480965,0.000020325395,0.000017071749,0.000023910714],"domain_scores_gemma":[0.9998615,0.000009892228,0.000054633485,0.000010692602,0.000028107626,0.00003519127],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000060704642,0.00016063999,0.00021236045,0.00066162273,0.0004099831,0.00026223308,0.00021118266,0.00023280754,0.00052956503],"category_scores_gemma":[0.00025932136,0.000128021,0.00011239657,0.0005251394,0.00029853938,0.0001932548,0.000289307,0.00014909416,0.00008258547],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023775658,0.000035782978,0.9164612,0.00005648694,0.000043050364,0.000774491,0.0008755426,0.0015692137,0.07187832,0.00007555791,0.00017314851,0.007819453],"study_design_scores_gemma":[0.0000010615834,0.000015227953,0.9985285,0.0000015631537,0.0000039183765,0.0000620857,0.00008585437,0.00057543867,0.0006408505,0.000004380287,0.00007884566,0.0000022665067],"about_ca_topic_score_codex":0.029660895,"about_ca_topic_score_gemma":0.07533538,"teacher_disagreement_score":0.029660895,"about_ca_system_score_codex":0.0005077989,"about_ca_system_score_gemma":0.00020883509,"threshold_uncertainty_score":0.05897647},"labels":[],"label_agreement":null},{"id":"W2508565385","doi":"10.1002/2015jb012604","title":"Deformation in the asthenospheric mantle beneath the Carpathian‐Pannonian Region","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological Formations and Processes Exploration","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"Austrian Science Fund","keywords":"Geology; Lithosphere; Tectonics; Mantle (geology); Seismology; Seismic anisotropy; Pannonian basin; Anisotropy; Shear (geology); Subduction; Shear zone; Geophysics; Paleontology","score_opus":0.05946834018141969,"score_gpt":0.30329345492601706,"score_spread":0.24382511474459737,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2508565385","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985757,0.00007305393,0.000055609635,0.000011079105,9.266765e-7,0.0000026947478,0.00011244431,0.0000056762024,0.0011628178],"genre_scores_gemma":[0.9996556,0.0000437727,0.00006513399,0.000002176419,8.804437e-7,0.0000021765186,0.00009184953,0.0000011283579,0.0001373753],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999567,0.0000038559165,0.0000036262388,0.00001782609,0.000007693289,0.00001025649],"domain_scores_gemma":[0.999905,0.000013730746,0.00003278651,0.000008690302,0.000028848464,0.000010922672],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012504004,0.0002682835,0.00012343375,0.0009194508,0.00031723225,0.00044746557,0.0001716036,0.00019831027,0.0010629912],"category_scores_gemma":[0.00021885199,0.0000954081,0.00013066946,0.001318874,0.00034179338,0.0002065794,0.00027458085,0.00010429386,0.000091566355],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004095757,0.000022394137,0.87393534,0.00010251166,0.00011030037,0.0011360177,0.001543248,0.0046379613,0.081528105,0.00035347758,0.00026710707,0.0359539],"study_design_scores_gemma":[0.0000022886222,0.000007077625,0.99879044,0.000003809011,0.0000057907755,0.00005328878,0.00012142919,0.00049285684,0.0002882328,0.00001813374,0.00021403407,0.000002511552],"about_ca_topic_score_codex":0.08100514,"about_ca_topic_score_gemma":0.08987291,"teacher_disagreement_score":0.08100514,"about_ca_system_score_codex":0.00066675316,"about_ca_system_score_gemma":0.00035123766,"threshold_uncertainty_score":0.1610673},"labels":[],"label_agreement":null},{"id":"W2508595123","doi":"10.1002/2016jb013194","title":"Crustal structure of the Kermadec arc from MANGO seismic refraction profiles","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ocean Networks Canada Society; University of Victoria","funders":"University of California, San Diego; National Geospatial-Intelligence Agency; University of Oxford; Natural Environment Research Council; Sight Research UK","keywords":"Geology; Trough (economics); Seismology; Subduction; Island arc; Neogene; Ridge; Tectonics; Seismic refraction; Trench; Discontinuity (linguistics); Inversion (geology); Paleontology","score_opus":0.022722756822676302,"score_gpt":0.2758251620470459,"score_spread":0.25310240522436955,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2508595123","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99760205,0.000072515846,0.000096704345,0.000011695698,0.0000011838196,0.0000041855337,0.00027118713,0.000017876977,0.0019225036],"genre_scores_gemma":[0.9993824,0.000039018418,0.00017646479,0.0000021294709,0.0000011330415,0.0000018063591,0.0002447437,0.000003859866,0.00014828186],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999498,0.0000023360715,0.0000034076106,0.0000136418075,0.000014166215,0.000016594695],"domain_scores_gemma":[0.99988735,0.000011817091,0.000035706686,0.000009883846,0.00003800957,0.000017140115],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006799235,0.00020091161,0.00011986231,0.0011719089,0.00020207395,0.000540183,0.00015061162,0.00013021509,0.0008264372],"category_scores_gemma":[0.00036768964,0.00013475896,0.00015241027,0.000704315,0.00016620258,0.00016156859,0.00039173578,0.0001250119,0.00016723013],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016092754,0.000025814788,0.9321673,0.00007848369,0.00010972954,0.00057605637,0.0007440387,0.0049682283,0.028153192,0.0003735479,0.0003210998,0.03232158],"study_design_scores_gemma":[0.000003617563,0.000004266301,0.99753964,0.000011594122,0.000012482003,0.000046584075,0.00013625881,0.0012287762,0.00052126433,0.000032822096,0.0004582913,0.0000043215127],"about_ca_topic_score_codex":0.047935486,"about_ca_topic_score_gemma":0.09535249,"teacher_disagreement_score":0.047935486,"about_ca_system_score_codex":0.00054875587,"about_ca_system_score_gemma":0.00040161386,"threshold_uncertainty_score":0.09531295},"labels":[],"label_agreement":null},{"id":"W2512144736","doi":"10.1002/2016jb013165","title":"Numerical upscaling in 2‐D heterogeneous poroelastic rocks: Anisotropic attenuation and dispersion of seismic waves","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":84,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Université de Lausanne; Kommission für Technologie und Innovation; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; National Science Foundation","keywords":"Poromechanics; Attenuation; Anelastic attenuation factor; Anisotropy; Seismic anisotropy; Seismic wave; Dissipation; Geology; Dispersive body waves; Dispersion (optics); Mechanics; Wave propagation; Stiffness matrix; Porous medium; Geophysics; Stiffness; Geotechnical engineering; Porosity; Physics; Optics","score_opus":0.024561995994170135,"score_gpt":0.2914658620021334,"score_spread":0.2669038660079633,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2512144736","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.69623953,0.00012178814,0.3015349,0.00007634795,0.000028284108,0.000059768317,0.000088278706,0.00069618,0.0011549429],"genre_scores_gemma":[0.92379445,0.000043416778,0.07582315,0.000008492146,0.0000053859494,0.000025187637,0.00006967062,0.00004133694,0.00018894584],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998348,0.00003750846,0.00001599099,0.000025492873,0.00007024846,0.000016015074],"domain_scores_gemma":[0.9990482,0.00044289322,0.00015000232,0.00017159908,0.00014635324,0.000040874937],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006264016,0.0005512943,0.00039954775,0.00058325013,0.00021839922,0.00052735227,0.0005490528,0.00046476917,0.0006433038],"category_scores_gemma":[0.0019023583,0.00019558663,0.000428859,0.0004769744,0.0005230458,0.00040019274,0.00043769914,0.0003826983,0.00007775772],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010387574,0.00011539938,0.0032412112,0.00009860866,0.00003845467,0.00015607923,0.00013474286,0.9073625,0.056038957,0.0015715989,0.00009263948,0.031046012],"study_design_scores_gemma":[0.0000038303415,0.000020550919,0.0003314303,0.0000021923715,0.0000023065145,0.000009902394,0.0000092512655,0.9947131,0.004704695,0.0001337254,0.00006436299,0.0000045149286],"about_ca_topic_score_codex":0.0031066742,"about_ca_topic_score_gemma":0.0021653683,"teacher_disagreement_score":0.0031066742,"about_ca_system_score_codex":0.00032735922,"about_ca_system_score_gemma":0.0003686944,"threshold_uncertainty_score":0.006177187},"labels":[],"label_agreement":null},{"id":"W2515592211","doi":"10.1002/2016jb013085","title":"Characteristics of slow earthquakes in the very low frequency band: Application to the Cascadia subduction zone","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Japan Society for the Promotion of Science","keywords":"Seismology; Subduction; Geology; Very low frequency; Seismogram; Seismometer; Episodic tremor and slip; Frequency band; Geophysics; Geodesy; Tectonics; Bandwidth (computing); Physics","score_opus":0.02510652625031032,"score_gpt":0.29085429085960945,"score_spread":0.2657477646092991,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2515592211","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966091,0.0001075942,0.0021084314,0.00004936518,0.000005379089,0.000009135882,0.00036914484,0.00011825805,0.0006236726],"genre_scores_gemma":[0.9985505,0.00004514842,0.0009257032,0.0000030592257,0.0000047143913,0.0000030087824,0.00033187258,0.000009414742,0.00012656488],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999899,0.000015745827,0.000010605056,0.0000319671,0.000026798863,0.00001577646],"domain_scores_gemma":[0.9995536,0.00011131816,0.00008464166,0.00007676248,0.0001034709,0.00007024412],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032060652,0.00052898005,0.00027626904,0.0018635526,0.00034511712,0.00041239476,0.00033342338,0.00036905467,0.00082701305],"category_scores_gemma":[0.0010089971,0.00017484,0.00032324228,0.0017497421,0.00023516451,0.00017316444,0.00039603963,0.00019499507,0.00019146563],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00051966595,0.00023713821,0.7559514,0.00026252164,0.00028014794,0.0021057366,0.0012602997,0.046237797,0.10582195,0.0002890229,0.0010025243,0.08603174],"study_design_scores_gemma":[0.000024025787,0.00009408557,0.9462613,0.000012310814,0.00007606976,0.0001954534,0.00028619583,0.04843151,0.0036556933,0.0001838275,0.00075252383,0.000027049884],"about_ca_topic_score_codex":0.019864423,"about_ca_topic_score_gemma":0.02205592,"teacher_disagreement_score":0.019864423,"about_ca_system_score_codex":0.00027139697,"about_ca_system_score_gemma":0.00024596442,"threshold_uncertainty_score":0.039497554},"labels":[],"label_agreement":null},{"id":"W2516764388","doi":"10.1002/2016jb012981","title":"An efficient repeating signal detector to investigate earthquake swarms","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Seismology; Induced seismicity; Seismometer; Geology; Volcano; Earthquake swarm; Waveform; Computer science","score_opus":0.04896967192179296,"score_gpt":0.3255477969576598,"score_spread":0.2765781250358668,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2516764388","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.19552408,0.00017879906,0.7971569,0.00010919391,0.000060937546,0.00013458493,0.00084854016,0.003922314,0.0020646907],"genre_scores_gemma":[0.4361513,0.00007942846,0.5605903,0.00004807482,0.000022831347,0.00011522052,0.0014114091,0.00011013749,0.001471331],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997322,0.000033323904,0.000021700456,0.000064604086,0.00011564601,0.000032531818],"domain_scores_gemma":[0.99916863,0.00028290026,0.00009325182,0.000107367014,0.00027635007,0.00007153637],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004973998,0.00046776189,0.0005142586,0.0022935627,0.00027772336,0.00047670555,0.0007060304,0.0003749845,0.0017192813],"category_scores_gemma":[0.0017936904,0.00025909278,0.0002835071,0.0014647781,0.0001960682,0.00042436022,0.00073318323,0.0002598203,0.0008661815],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00054095447,0.00028271863,0.037197612,0.00022118528,0.00017247454,0.00045598418,0.0002494178,0.07456068,0.22571914,0.00406156,0.0063435775,0.6501947],"study_design_scores_gemma":[0.000043390628,0.00015678183,0.009571012,0.000008444797,0.000024867431,0.00022732723,0.00009641608,0.9561872,0.028729657,0.0012326778,0.0036931909,0.00002900396],"about_ca_topic_score_codex":0.0020851744,"about_ca_topic_score_gemma":0.003643675,"teacher_disagreement_score":0.0022935627,"about_ca_system_score_codex":0.00031430848,"about_ca_system_score_gemma":0.0007996087,"threshold_uncertainty_score":0.00575161},"labels":[],"label_agreement":null},{"id":"W2521540026","doi":"10.1002/2016jb013460","title":"Identifying mantle lithosphere inheritance in controlling intraplate orogenesis","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"University of Toronto; Canada Foundation for Innovation","keywords":"Lithosphere; Intraplate earthquake; Geology; Mantle (geology); Collision zone; Plate tectonics; Geophysics; Hotspot (geology); Tectonics; Seismology","score_opus":0.045762826280324194,"score_gpt":0.32314579051396985,"score_spread":0.27738296423364567,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2521540026","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977888,0.00003565309,0.0017942938,0.000013788962,0.0000010825305,0.0000023298053,0.0000206146,0.000015066739,0.00032840765],"genre_scores_gemma":[0.9996561,0.000009813904,0.00029572056,0.0000015342848,2.0087624e-7,6.8183994e-7,0.000009012257,0.0000018745174,0.000025078469],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999168,0.000021593965,0.0000060154894,0.000024521963,0.000012486692,0.000018594012],"domain_scores_gemma":[0.99965835,0.00013691437,0.000082233084,0.00005374248,0.000025632684,0.000043148302],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003098749,0.00023529057,0.00024265308,0.0004418841,0.00017952865,0.0006302864,0.0003437449,0.00033056308,0.0008617066],"category_scores_gemma":[0.0014142778,0.00018450357,0.0001889916,0.00031698434,0.00048747036,0.00041083328,0.00043003573,0.00024048804,0.00006954684],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006055185,0.00013718933,0.41906962,0.00019727917,0.00023583915,0.00042588555,0.00032996322,0.22299054,0.32496345,0.0047454387,0.00015090554,0.026148371],"study_design_scores_gemma":[0.0000423209,0.00023062988,0.33485565,0.00002922213,0.00009601801,0.00014275336,0.0002837195,0.6267229,0.03339516,0.003731132,0.0004340321,0.0000364273],"about_ca_topic_score_codex":0.0028413488,"about_ca_topic_score_gemma":0.0025776546,"teacher_disagreement_score":0.0028413488,"about_ca_system_score_codex":0.0002953181,"about_ca_system_score_gemma":0.00022326688,"threshold_uncertainty_score":0.0056496263},"labels":[],"label_agreement":null},{"id":"W2523144424","doi":"10.1002/2016jb013173","title":"A method for determining transverse permeability of tight reservoir cores by radial pressure pulse decay measurement","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"National Natural Science Foundation of China","keywords":"Transverse plane; Mechanics; Volume (thermodynamics); Permeability (electromagnetism); Surface-area-to-volume ratio; Approximation error; Observational error; Mathematics; Materials science; Physics; Mathematical analysis; Chemistry; Thermodynamics; Statistics; Structural engineering; Engineering","score_opus":0.05652879452271322,"score_gpt":0.3445171839591665,"score_spread":0.2879883894364533,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2523144424","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.022992691,0.00036825368,0.9754311,0.00004810201,0.000034429057,0.000054118198,0.000079630576,0.0004940229,0.0004976159],"genre_scores_gemma":[0.37167928,0.00074832415,0.62566257,0.00006804442,0.000028984892,0.0002637927,0.0001509093,0.000090002475,0.0013080316],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9991835,0.00015317193,0.000037602003,0.00018261961,0.00040777776,0.00003532061],"domain_scores_gemma":[0.9988231,0.00044277738,0.00018420005,0.00014356559,0.00035899496,0.000047356003],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010854654,0.0006629602,0.0005868865,0.0010228159,0.00031550726,0.0005313496,0.00086464203,0.00061897293,0.0009858828],"category_scores_gemma":[0.002246313,0.00045898947,0.00033912473,0.0007061034,0.00047163517,0.0012781596,0.0008413574,0.0009354901,0.0004036177],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015593326,0.00005111034,0.0020817888,0.00044787463,0.000023961264,0.00010796661,0.00012803866,0.0043608127,0.8768321,0.002894349,0.0004342813,0.11248177],"study_design_scores_gemma":[0.000030710275,0.00033931326,0.003028477,0.000039159608,0.000045370096,0.00052533374,0.00007629792,0.2290149,0.76128006,0.0015767483,0.003939372,0.00010429823],"about_ca_topic_score_codex":0.00062257785,"about_ca_topic_score_gemma":0.0006499072,"teacher_disagreement_score":0.0010854654,"about_ca_system_score_codex":0.00039884716,"about_ca_system_score_gemma":0.0006401467,"threshold_uncertainty_score":0.0057405233},"labels":[],"label_agreement":null},{"id":"W2529847781","doi":"10.1002/2016jb013154","title":"An assessment of forward and inverse GIA solutions for Antarctica","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":66,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"British Antarctic Survey; National Centre for Earth Observation; Natural Environment Research Council; Jet Propulsion Laboratory; University of Bristol; Australian Research Council; Sight Research UK; University of Toronto; National Aeronautics and Space Administration; National Science Foundation","keywords":"Geology; Post-glacial rebound; Ice sheet; Peninsula; Lithosphere; Geodesy; Mantle (geology); Oceanography; Geophysics; Seismology; Geography; Tectonics","score_opus":0.0815000241690594,"score_gpt":0.3896473758319211,"score_spread":0.3081473516628617,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2529847781","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8306452,0.007388284,0.12942111,0.0020779064,0.00045326425,0.00009427021,0.003650987,0.0018292621,0.02443963],"genre_scores_gemma":[0.8855869,0.001257393,0.107797645,0.00013714796,0.00014702047,0.000044217453,0.0029967187,0.000388572,0.0016443424],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9990513,0.0002558871,0.00011055029,0.00017572043,0.00034419255,0.00006241994],"domain_scores_gemma":[0.9964478,0.00092030485,0.0005261319,0.0005255812,0.0014882366,0.00009190725],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.003961986,0.00067617977,0.0003964724,0.0026272247,0.00057587575,0.0017416227,0.0006481894,0.0006778787,0.0013353983],"category_scores_gemma":[0.014866036,0.00045692112,0.00084401004,0.0020681531,0.00032318066,0.0015141951,0.0011731504,0.000671778,0.00064195093],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034021688,0.00006211544,0.36634183,0.00054320146,0.00070295425,0.00020212431,0.001064709,0.1579507,0.009348024,0.008133745,0.0042809676,0.45102942],"study_design_scores_gemma":[0.0001382366,0.00022034561,0.49856445,0.00053323107,0.00035311808,0.0008233023,0.0010686495,0.42711887,0.011670008,0.009470902,0.049794972,0.0002439085],"about_ca_topic_score_codex":0.012600565,"about_ca_topic_score_gemma":0.013508306,"teacher_disagreement_score":0.012600565,"about_ca_system_score_codex":0.0007142958,"about_ca_system_score_gemma":0.0013677465,"threshold_uncertainty_score":0.025054455},"labels":[],"label_agreement":null},{"id":"W2530253103","doi":"10.1002/2016jb013043","title":"Inferences of mantle viscosity based on ice age data sets: Radial structure","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":110,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"Division of Ocean Sciences; Harvard University; National Science Foundation","keywords":"Post-glacial rebound; Mantle (geology); Geology; Geopotential; Geodetic datum; Geodesy; Geophysics; Viscosity; Sea level; Thermodynamics; Physics; Oceanography","score_opus":0.10896146655382628,"score_gpt":0.35201997068113244,"score_spread":0.24305850412730617,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2530253103","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99574137,0.0000477755,0.00285568,0.000022020608,0.0000019908812,0.0000038915823,0.00043502575,0.00007723141,0.0008150159],"genre_scores_gemma":[0.9970091,0.000019587796,0.0022632729,0.0000035163557,0.0000023821028,0.0000025670477,0.0006034868,0.0000151008935,0.000081027334],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998287,0.00005244868,0.0000125066845,0.00003809912,0.00003715506,0.00003108373],"domain_scores_gemma":[0.9988426,0.00049546116,0.00018267396,0.00015210874,0.00024041875,0.00008677481],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010933138,0.00033384928,0.00026623308,0.0014947597,0.00031153552,0.0007420551,0.00029992816,0.00021739368,0.00055809226],"category_scores_gemma":[0.005786468,0.0002760984,0.0004787906,0.00087840937,0.0002624812,0.000403566,0.00038869533,0.00034386403,0.0002455773],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032080497,0.00005060246,0.88935286,0.000023375333,0.00022693399,0.000070557784,0.00023976644,0.0605736,0.020313716,0.00083992013,0.00029299938,0.027694749],"study_design_scores_gemma":[0.000027140506,0.000038246446,0.68417466,0.000018836685,0.000077248005,0.000043912918,0.00013959929,0.30636278,0.007370203,0.00081549666,0.0008934397,0.000038469512],"about_ca_topic_score_codex":0.028187158,"about_ca_topic_score_gemma":0.029813388,"teacher_disagreement_score":0.028187158,"about_ca_system_score_codex":0.00044920112,"about_ca_system_score_gemma":0.000481498,"threshold_uncertainty_score":0.056046188},"labels":[],"label_agreement":null},{"id":"W2537607085","doi":"10.1002/2016jb013244","title":"Distinct crustal structure of the North American Midcontinent Rift from <i>P</i> wave receiver functions","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal; University of Manitoba","funders":"Northwestern University; National Science Foundation","keywords":"Geology; Rift; Seismology; Bouguer anomaly; Receiver function; Terrane; Crust; Archean; Underplating; Fault (geology); Gravity anomaly; Tectonics; Geophysics; Paleontology; Lithosphere","score_opus":0.02701380788038219,"score_gpt":0.2693459747573953,"score_spread":0.24233216687701312,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2537607085","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984812,0.00007868411,0.00015018179,0.000020384625,0.0000011930837,0.0000014205264,0.00032527308,0.00001558395,0.0009261635],"genre_scores_gemma":[0.99898344,0.000029304667,0.00010848588,0.0000060374196,0.0000017653654,0.0000012165063,0.000580533,0.0000031205323,0.00028609627],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996054,0.000004732123,0.000001814928,0.000011795988,0.000009671113,0.000011470009],"domain_scores_gemma":[0.99975175,0.000035507313,0.000053404914,0.000016711047,0.000101654856,0.000040964034],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012805531,0.00014478216,0.00007177383,0.0005483269,0.00017805658,0.00036592266,0.00012858109,0.00012395073,0.0014518477],"category_scores_gemma":[0.00035221005,0.00009807096,0.000080945945,0.00037180577,0.00011265324,0.00016130292,0.00021603944,0.0001098858,0.00022362116],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000075611424,0.000022718888,0.942202,0.000023895382,0.000042229673,0.00024222738,0.0005540512,0.00065854273,0.029643618,0.00013226364,0.0005362346,0.025866603],"study_design_scores_gemma":[5.38628e-7,0.000003950924,0.9993591,0.000001586353,0.0000030888841,0.000020486816,0.00003397872,0.00026697494,0.00011736735,0.0000048274037,0.00018714994,9.202206e-7],"about_ca_topic_score_codex":0.032103647,"about_ca_topic_score_gemma":0.067816846,"teacher_disagreement_score":0.032103647,"about_ca_system_score_codex":0.00018783844,"about_ca_system_score_gemma":0.00018907903,"threshold_uncertainty_score":0.063833594},"labels":[],"label_agreement":null},{"id":"W2552026601","doi":"10.1002/2016jb013285","title":"Interaction between the supercontinent cycle and the evolution of intrinsically dense provinces in the deep mantle","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Supercontinent; Mantle (geology); Geology; Mantle convection; Mantle plume; Earth science; Lithosphere; Geophysics; Craton; Paleontology; Tectonics","score_opus":0.018507438327752986,"score_gpt":0.27568816366720394,"score_spread":0.25718072533945097,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2552026601","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99966025,0.0000097670445,0.00013366077,0.000008855733,4.1875043e-7,6.814067e-7,0.000021464697,0.0000045047095,0.00016030882],"genre_scores_gemma":[0.9998598,0.0000061683945,0.000083460174,0.0000013779625,3.7407514e-7,6.632819e-7,0.000019646503,0.0000019786082,0.000026554553],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999472,0.000014814954,0.0000023284765,0.000013832028,0.0000071982104,0.000014611917],"domain_scores_gemma":[0.99966216,0.00013614721,0.000071699804,0.0000417929,0.00003290944,0.000055238175],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019948817,0.00016978852,0.00017356449,0.0004500182,0.00035490328,0.0007288283,0.00034951823,0.00022919466,0.00078044075],"category_scores_gemma":[0.0008766534,0.00018534677,0.00031067745,0.0003246834,0.00048185105,0.00021760231,0.0005593312,0.00025105895,0.000053569333],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034755663,0.00008808987,0.754953,0.000028259696,0.00017684611,0.00037867567,0.00026102396,0.21053097,0.023441574,0.0033920081,0.00020921114,0.006192784],"study_design_scores_gemma":[0.000051641964,0.00011386001,0.50838333,0.000006820273,0.00006248148,0.00014376202,0.0002665082,0.4860938,0.0026937816,0.0016612748,0.0004967001,0.00002592789],"about_ca_topic_score_codex":0.01261745,"about_ca_topic_score_gemma":0.008803558,"teacher_disagreement_score":0.01261745,"about_ca_system_score_codex":0.00055049884,"about_ca_system_score_gemma":0.00025548218,"threshold_uncertainty_score":0.025088012},"labels":[],"label_agreement":null},{"id":"W2557168806","doi":"10.1002/2016jb013534","title":"Advanced seismic imaging techniques characterize the Alpine Fault at Whataroa (New Zealand)","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"University of Alberta; German-Israeli Foundation for Scientific Research and Development; University of Otago","keywords":"Geology; Seismology; Fault (geology); Basement; Borehole; Reflector (photography); Reflection (computer programming); Drilling; Paleontology","score_opus":0.02895352837546385,"score_gpt":0.30713471931117325,"score_spread":0.2781811909357094,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2557168806","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9938524,0.0001751765,0.001130253,0.000046286215,0.000004015761,0.000034560777,0.0008113639,0.000041417083,0.0039044742],"genre_scores_gemma":[0.9933295,0.0002066613,0.0035739657,0.000015832078,0.000005728674,0.00002138051,0.0007993097,0.000016505765,0.0020311696],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990165,0.0000039677957,0.0000050379404,0.000024594852,0.000044084092,0.000020634447],"domain_scores_gemma":[0.99981564,0.000013581813,0.00006476518,0.000010765699,0.00006955397,0.000025741574],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014594744,0.00029346094,0.00011909262,0.0014845338,0.00023903439,0.00057560555,0.00025629363,0.00027568042,0.001913385],"category_scores_gemma":[0.0004355118,0.00020029972,0.00013390332,0.0009344158,0.00023731377,0.00037801036,0.00033395115,0.00023625989,0.00033997514],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032083425,0.0001547988,0.4446076,0.00024734304,0.00008227718,0.0010290678,0.002097391,0.0036330814,0.42448625,0.00039485178,0.0013737723,0.12157268],"study_design_scores_gemma":[0.00001598196,0.000043247735,0.99162793,0.000015284482,0.000014333652,0.00018725914,0.00040273648,0.0033326629,0.0025903,0.00003888362,0.0017222658,0.00000918907],"about_ca_topic_score_codex":0.14470936,"about_ca_topic_score_gemma":0.30987972,"teacher_disagreement_score":0.14470936,"about_ca_system_score_codex":0.00058195327,"about_ca_system_score_gemma":0.00037796568,"threshold_uncertainty_score":0.2877341},"labels":[],"label_agreement":null},{"id":"W2560560141","doi":"10.1002/2016jb013123","title":"3‐D velocity structure in southern Haiti from local earthquake tomography","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Resources Canada; U.S. Geological Survey; Institut de Physique du Globe de Paris; Centre National de la Recherche Scientifique; Institut Français de Recherche pour l'Exploitation de la Mer","keywords":"Geology; Seismology; Aftershock; Hypocenter; Fault (geology); Submarine pipeline; Structural basin; Peninsula; Seismometer; Seismic tomography; Geomorphology; Induced seismicity; Paleontology; Oceanography; Geography","score_opus":0.028215322223662815,"score_gpt":0.28475677498635843,"score_spread":0.25654145276269563,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2560560141","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984471,0.000026843685,0.0005429759,0.000022708362,0.0000013819533,0.000007537273,0.00027261305,0.00003233702,0.00064648234],"genre_scores_gemma":[0.99860114,0.000027471768,0.0006898615,0.0000054105953,0.0000019681881,0.000005500068,0.0004560417,0.000004594659,0.00020799773],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999962,0.0000035846324,0.0000023547368,0.000011168808,0.000009943003,0.000010982572],"domain_scores_gemma":[0.9998727,0.000016381104,0.000040237934,0.000010791086,0.00004221969,0.000017606686],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010118916,0.0002504569,0.000118310694,0.0009693948,0.00023607704,0.00051849097,0.00022669682,0.00023915566,0.00061798265],"category_scores_gemma":[0.00040457945,0.00018699729,0.00015718292,0.0009168368,0.0002459236,0.00024284355,0.00031960098,0.00017335858,0.0001506217],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028402734,0.00014004036,0.89101964,0.00009003145,0.000110749024,0.0011449546,0.0014256012,0.019244207,0.049341,0.0005036191,0.00075988716,0.035936248],"study_design_scores_gemma":[0.0000134980255,0.00003108968,0.96512026,0.00001428121,0.000036576632,0.00022886923,0.00056470756,0.030691124,0.0025950489,0.00006095417,0.0006270524,0.00001658888],"about_ca_topic_score_codex":0.054769643,"about_ca_topic_score_gemma":0.13344266,"teacher_disagreement_score":0.054769643,"about_ca_system_score_codex":0.00040533434,"about_ca_system_score_gemma":0.0005419907,"threshold_uncertainty_score":0.10890168},"labels":[],"label_agreement":null},{"id":"W2560600136","doi":"10.1002/2016jb013570","title":"A seismological overview of the induced earthquakes in the Duvernay play near Fox Creek, Alberta","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":189,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University; University of Alberta","funders":"","keywords":"Geology; Seismology; Hydraulic fracturing; Induced seismicity; Lineament; Focal mechanism; Precambrian; Stress field; Basement; Fault (geology); Paleontology; Tectonics; Geography","score_opus":0.10442221959556322,"score_gpt":0.3443423533590797,"score_spread":0.23992013376351648,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2560600136","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98057556,0.0018311098,0.0006139158,0.00017701383,0.000008288029,0.00004773959,0.0026666776,0.00004394719,0.014035776],"genre_scores_gemma":[0.99162185,0.001470501,0.00075014716,0.00003745774,0.0000089085825,0.000009417185,0.0013007885,0.0000066348584,0.004794442],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987066,0.0000067913807,0.000006035473,0.00001916179,0.00006136294,0.00003587043],"domain_scores_gemma":[0.9996854,0.000031080996,0.00005087223,0.0000086424625,0.0001655523,0.000058468653],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001630542,0.00021208102,0.00013630408,0.0034502132,0.00086883287,0.00085834344,0.00041616333,0.00016096597,0.0014983916],"category_scores_gemma":[0.00035022717,0.00010467805,0.000088994246,0.0037780113,0.00042261402,0.00012578937,0.00039630913,0.000118626434,0.00014118674],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000113199676,0.000042414104,0.9101196,0.00018648757,0.00005518237,0.0010054399,0.004594866,0.002569151,0.012686815,0.0011065817,0.0019347287,0.06558559],"study_design_scores_gemma":[0.0000014430843,0.000012803778,0.99301296,0.000017378217,0.000008489465,0.000100877936,0.0015969484,0.0004324739,0.0002894837,0.000043279695,0.004478336,0.0000056662097],"about_ca_topic_score_codex":0.92652845,"about_ca_topic_score_gemma":0.9812531,"teacher_disagreement_score":0.073471546,"about_ca_system_score_codex":0.006067927,"about_ca_system_score_gemma":0.0042216014,"threshold_uncertainty_score":0.14780843},"labels":[],"label_agreement":null},{"id":"W2575768900","doi":"10.1002/2016jb013405","title":"On corner frequencies, attenuation, and low‐frequency earthquakes","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Attenuation; Geology; Seismology; Seismogram; Frequency band; Saturation (graph theory); Anelastic attenuation factor; Physics; Geodesy; Optics; Mathematics; Bandwidth (computing); Telecommunications","score_opus":0.05683777357723818,"score_gpt":0.3289944415736522,"score_spread":0.272156667996414,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2575768900","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8919513,0.0079837935,0.087865,0.0003364128,0.000023967741,0.000025402136,0.0002772915,0.00012263954,0.011414236],"genre_scores_gemma":[0.99433494,0.0014422501,0.003378693,0.00003009702,0.000033881777,0.000005578476,0.00008787468,0.000015874119,0.0006708704],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999634,0.00008725599,0.000021019709,0.00007554337,0.00014976187,0.000032397573],"domain_scores_gemma":[0.99134266,0.0065121395,0.00095665856,0.00032602725,0.00075599726,0.00010657321],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013119733,0.00026971873,0.0003311157,0.002091998,0.00021681118,0.0007279536,0.00045785375,0.00039279336,0.0013935148],"category_scores_gemma":[0.009526777,0.00019314833,0.00013274237,0.0017481262,0.0012432608,0.0009195357,0.00067281816,0.0004138107,0.00021071383],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00063977356,0.000074185016,0.4678002,0.001189227,0.00017406775,0.0020458337,0.003196332,0.072870195,0.05419889,0.074701495,0.001693721,0.32141602],"study_design_scores_gemma":[0.0000125143015,0.00016839246,0.8297004,0.00030137302,0.00007542449,0.00094381324,0.0010563293,0.08694198,0.013886109,0.05880124,0.008005419,0.00010702156],"about_ca_topic_score_codex":0.009112414,"about_ca_topic_score_gemma":0.008831601,"teacher_disagreement_score":0.009112414,"about_ca_system_score_codex":0.00071124866,"about_ca_system_score_gemma":0.00019623783,"threshold_uncertainty_score":0.01811874},"labels":[],"label_agreement":null},{"id":"W2586342266","doi":"10.1002/2016jb013430","title":"Deformation pattern during normal faulting: A sequential limit analysis","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"China Scholarship Council","keywords":"Geology; Echelon formation; Graben; Wedge (geometry); Fault (geology); Seismology; Detachment fault; Rotation (mathematics); Half-graben; Tectonics; Geometry","score_opus":0.0621319999010266,"score_gpt":0.34304792310465804,"score_spread":0.28091592320363146,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2586342266","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.86251575,0.00026319228,0.12596042,0.00031368315,0.000019146011,0.000040724328,0.00018200674,0.00023347806,0.010471728],"genre_scores_gemma":[0.9950617,0.000082112274,0.0029490981,0.000012485123,0.0000075227276,0.000028805487,0.000038985905,0.000025060195,0.0017943112],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99987483,0.00003594091,0.000008508106,0.000030277984,0.000029529696,0.00002085716],"domain_scores_gemma":[0.99971944,0.00009239792,0.000075182616,0.000026550624,0.00004087187,0.000045463956],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045663206,0.0004424268,0.00046776547,0.0007687829,0.00040372874,0.0007583068,0.0010258798,0.00069658936,0.0021018232],"category_scores_gemma":[0.001140828,0.00037437014,0.0007436135,0.00046215532,0.0011405754,0.0007224948,0.000696464,0.00038110185,0.00017393213],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021424932,0.000022229782,0.00234643,0.000011993315,0.000014262121,0.0001139197,0.000036387595,0.9841739,0.0013613089,0.010134007,0.000094933624,0.0016691827],"study_design_scores_gemma":[0.000003877283,0.000007235854,0.00026073557,0.000001116978,0.000002697369,0.000011184602,0.0000035512421,0.99796593,0.00008731898,0.0015629624,0.000090840855,0.0000025116456],"about_ca_topic_score_codex":0.014331452,"about_ca_topic_score_gemma":0.0040801642,"teacher_disagreement_score":0.014331452,"about_ca_system_score_codex":0.0011020986,"about_ca_system_score_gemma":0.00053937297,"threshold_uncertainty_score":0.028496087},"labels":[],"label_agreement":null},{"id":"W2594231710","doi":"10.1002/2016jb013778","title":"Modeling slow‐slip segmentation in Cascadia subduction zone constrained by tremor locations and gravity anomalies","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Geology; Subduction; Seismology; Episodic tremor and slip; Slip (aerodynamics); Bouguer anomaly; Global Positioning System; Geodesy; Lithosphere; Slab; Gravity anomaly; Geophysics; Tectonics","score_opus":0.052653627948352634,"score_gpt":0.33678930101728943,"score_spread":0.2841356730689368,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2594231710","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9941512,0.000063844964,0.0035370335,0.00016006279,0.000010178075,0.000012391283,0.00028650896,0.00019547889,0.0015832855],"genre_scores_gemma":[0.99898165,0.000025881267,0.0004733153,0.000009494355,0.0000027206013,0.000008126431,0.00013346576,0.000014680414,0.00035059455],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99990094,0.000021534353,0.0000055818878,0.00003247215,0.000011089461,0.000028379029],"domain_scores_gemma":[0.9996524,0.00012464078,0.000054597585,0.000029584118,0.000045265017,0.000093583025],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028445665,0.0009041107,0.00048688176,0.000560602,0.00060306303,0.0008377542,0.0010420792,0.0012487284,0.0016227684],"category_scores_gemma":[0.00090999703,0.0007241081,0.0007870717,0.00043212142,0.0007020366,0.00035014338,0.00064023,0.00062836765,0.00015729821],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000025892328,0.000015807675,0.006619112,0.000005891139,0.000020631354,0.000050744347,0.000016998702,0.99235207,0.00040080707,0.000117558804,0.00006786693,0.00030660132],"study_design_scores_gemma":[0.000010534267,0.000009661856,0.002269098,0.0000015016319,0.0000069838397,0.0000038434846,0.000012761425,0.99748397,0.000057423702,0.000083862884,0.000056241104,0.000004066938],"about_ca_topic_score_codex":0.19702907,"about_ca_topic_score_gemma":0.107182845,"teacher_disagreement_score":0.19702907,"about_ca_system_score_codex":0.0020159704,"about_ca_system_score_gemma":0.0016030121,"threshold_uncertainty_score":0.39176446},"labels":[],"label_agreement":null},{"id":"W2599486791","doi":"10.1002/2016jb013835","title":"Nucleation of dynamic slip on a hydraulically fractured fault","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Hydraulic Fracturing and Reservoir Analysis","field":"Engineering","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Slip (aerodynamics); Slipping; Nucleation; Instability; Geology; Mechanics; Geotechnical engineering; Fault (geology); Shear (geology); Seismology; Structural engineering; Petrology; Engineering; Physics; Thermodynamics","score_opus":0.021453641167394018,"score_gpt":0.33727943118374754,"score_spread":0.3158257900163535,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2599486791","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9948395,0.00015219595,0.0031270708,0.000021377875,0.000008570503,0.000008648173,0.00005339657,0.000048052854,0.0017411611],"genre_scores_gemma":[0.9996567,0.000018712044,0.00016426816,0.0000021494905,0.0000031622021,0.000002276233,0.000020518437,0.0000025883926,0.0001294818],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998876,0.000010410533,0.0000064771043,0.000030717227,0.000026960823,0.00003795202],"domain_scores_gemma":[0.99957484,0.00017091681,0.00008424377,0.000025596613,0.000044031458,0.000100301804],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001700411,0.00017987787,0.0003646994,0.00041997145,0.00037506619,0.00049468456,0.0002553845,0.00024215895,0.0014308951],"category_scores_gemma":[0.00079555815,0.00016458202,0.00020805601,0.00010576842,0.00058946555,0.00028503165,0.00053293386,0.00022913437,0.00009885384],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010976475,0.00021046029,0.09419544,0.00035874665,0.00014481616,0.0054977587,0.00056608464,0.13055074,0.7228953,0.020084962,0.0008586676,0.02353948],"study_design_scores_gemma":[0.00008008945,0.00079037354,0.09687308,0.00004146242,0.000067142064,0.0014950378,0.00039372753,0.4579382,0.43371037,0.006752588,0.0017982017,0.000059718128],"about_ca_topic_score_codex":0.0010824399,"about_ca_topic_score_gemma":0.00048443887,"teacher_disagreement_score":0.0014308951,"about_ca_system_score_codex":0.0006486189,"about_ca_system_score_gemma":0.00019149247,"threshold_uncertainty_score":0.004786849},"labels":[],"label_agreement":null},{"id":"W2601538800","doi":"10.1002/2017jb013983","title":"Continental crust anisotropy measurements from tectonic tremor in Cascadia","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey","keywords":"Geology; Seismology; Tectonics; Crust; Anisotropy; Continental crust; Stress field; Shear wave splitting; Subduction; Continental margin; Passive margin; Aftershock; Geophysics; Shear (geology); Paleontology; Rift","score_opus":0.10644487521237204,"score_gpt":0.3560746163890352,"score_spread":0.24962974117666314,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2601538800","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972861,0.00004481059,0.00029825835,0.000019294735,0.0000027486278,0.0000029921669,0.00053270103,0.000061908126,0.0017512003],"genre_scores_gemma":[0.9992581,0.000029791772,0.00014212115,0.000002412081,0.0000016397793,0.0000026054015,0.00035602448,0.000005773746,0.00020139992],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987805,0.0000069861358,0.000008702026,0.000042305524,0.000045307414,0.000018671903],"domain_scores_gemma":[0.99965835,0.000027903972,0.00007664674,0.000032194737,0.00011955718,0.000085370935],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013978595,0.0004184284,0.00018817365,0.0013357716,0.0004970436,0.00037929774,0.0001794128,0.00016733812,0.0012488366],"category_scores_gemma":[0.00059889193,0.00020078599,0.00022080143,0.00097550754,0.00022433893,0.00017419833,0.00044197112,0.00022771867,0.00022210505],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024546622,0.000031183634,0.8779915,0.00004787292,0.0001286084,0.00033411907,0.0006762348,0.002536075,0.106331386,0.00008746617,0.00036372853,0.011226339],"study_design_scores_gemma":[0.0000031804482,0.000010562056,0.99776125,0.0000020895336,0.000011714065,0.000025838557,0.00008256677,0.00056581374,0.0012852703,0.000016851578,0.0002313373,0.0000035361218],"about_ca_topic_score_codex":0.048549652,"about_ca_topic_score_gemma":0.07572753,"teacher_disagreement_score":0.95145035,"about_ca_system_score_codex":0.0006957528,"about_ca_system_score_gemma":0.00028010842,"threshold_uncertainty_score":0.09653413},"labels":[],"label_agreement":null},{"id":"W2602772114","doi":"10.1002/2016jb013356","title":"Automated detection and cataloging of global explosive volcanism using the International Monitoring System infrasound network","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":64,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Resources Canada; National Science Foundation","keywords":"Infrasound; Explosive material; Explosive eruption; Warning system; SIGNAL (programming language); Computer science; Volcano; Hazard; Seismology; Geology; Volcanic hazards; Volcanism; Remote sensing; Real-time computing; Telecommunications; Magma; Acoustics; Geography","score_opus":0.05486887721328785,"score_gpt":0.34667164152191177,"score_spread":0.2918027643086239,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2602772114","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.89484286,0.00007345173,0.096731514,0.000115219606,0.00001612911,0.00010869073,0.0023252792,0.002126769,0.0036600882],"genre_scores_gemma":[0.89258105,0.000029900566,0.10389315,0.000015282058,0.000010780189,0.000045968303,0.0025843368,0.00005908281,0.0007804925],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997261,0.00005645597,0.000023601666,0.00008085479,0.00007910074,0.00003381247],"domain_scores_gemma":[0.998906,0.0003053965,0.00021970198,0.00018179277,0.0003238829,0.00006320945],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005890117,0.00032608493,0.0002510393,0.0018886664,0.00020564886,0.00050714397,0.00030593958,0.0001533685,0.0010358533],"category_scores_gemma":[0.0016910519,0.0001061713,0.00020764122,0.001120126,0.000120038225,0.00048907584,0.00055878266,0.00017545943,0.00030166082],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039895982,0.00023174469,0.49041814,0.000067084635,0.0001390811,0.00013851933,0.0003108803,0.054888703,0.034180034,0.0011426068,0.0037837669,0.41430056],"study_design_scores_gemma":[0.000047593167,0.00020611203,0.26656494,0.000016374139,0.00006859013,0.00015796423,0.00034026915,0.7007563,0.026061906,0.0009976028,0.004746424,0.0000359396],"about_ca_topic_score_codex":0.0114774825,"about_ca_topic_score_gemma":0.021400984,"teacher_disagreement_score":0.0114774825,"about_ca_system_score_codex":0.00033387475,"about_ca_system_score_gemma":0.0005365898,"threshold_uncertainty_score":0.022821307},"labels":[],"label_agreement":null},{"id":"W2602836083","doi":"10.1002/2017jb014048","title":"Microgravity changes at the Laguna del Maule volcanic field: Magma‐induced stress changes facilitate mass addition","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Geology; Dike; Magma; Sill; Volcano; Rock mass classification; Fault (geology); Petrology; Rhyolite; Deformation (meteorology); Stress field; Seismology; Silicic; Intrusion; Geochemistry; Volcanic rock; Geotechnical engineering","score_opus":0.08974914259721456,"score_gpt":0.33805599192339614,"score_spread":0.24830684932618158,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2602836083","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990677,0.000034604844,0.00008512357,0.000027028964,0.0000017490039,0.0000029163425,0.00013356944,0.00001882093,0.00062843534],"genre_scores_gemma":[0.9997008,0.000018848488,0.000057148885,0.0000044912085,0.0000017482505,0.000001726896,0.00006883289,0.0000018015248,0.00014465407],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996257,0.000003138374,0.0000019086501,0.000011730496,0.000006315329,0.000014308364],"domain_scores_gemma":[0.9999193,0.000010755486,0.000029956862,0.0000071001064,0.000012594298,0.00002026776],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000069068,0.00026147286,0.00011737567,0.00046017824,0.00018790024,0.00049244514,0.00023391514,0.00025518227,0.001699358],"category_scores_gemma":[0.0002752804,0.000121307654,0.0001909291,0.00034888703,0.00024494034,0.00036309042,0.0002718004,0.00012498806,0.00010289204],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021477562,0.000076913915,0.91541874,0.00007629725,0.00009765065,0.000680258,0.0005937173,0.012693037,0.057023298,0.0002847424,0.00048105733,0.012359531],"study_design_scores_gemma":[0.0000067858427,0.000018979257,0.99448013,0.000002847129,0.00000916944,0.00003191208,0.00016607156,0.003976886,0.0009694082,0.000046624387,0.00028570218,0.000005402118],"about_ca_topic_score_codex":0.017868528,"about_ca_topic_score_gemma":0.021422895,"teacher_disagreement_score":0.017868528,"about_ca_system_score_codex":0.0005875024,"about_ca_system_score_gemma":0.00028363662,"threshold_uncertainty_score":0.035529017},"labels":[],"label_agreement":null},{"id":"W2603784750","doi":"10.1002/2016jb013691","title":"Temporal variation of the shallow subsurface at the Aquistore CO<sub>2</sub> storage site associated with environmental influences using a continuous and controlled seismic source","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Petroleum Technology Research Centre","funders":"","keywords":"Geology; Environmental science; Soil science; Repeatability; Seismology; Atmospheric sciences; Hydrology (agriculture); Geotechnical engineering","score_opus":0.019917426482813833,"score_gpt":0.2640770215372151,"score_spread":0.24415959505440124,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2603784750","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99859804,0.000013994786,0.00044001857,0.000011906957,0.0000028157654,0.0000048566626,0.00049577584,0.000021922207,0.00041056916],"genre_scores_gemma":[0.9986754,0.000013200697,0.00056148303,0.000006188022,0.000002277986,0.000006740405,0.00052654,0.0000048554593,0.00020335936],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991536,0.000004399081,0.000003874087,0.000022165003,0.000032616532,0.00002149078],"domain_scores_gemma":[0.9997008,0.000025688738,0.00006519448,0.000011449557,0.0001589434,0.00003794772],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011181556,0.00020472094,0.00014764715,0.0006632152,0.00028291068,0.00029821252,0.00020027148,0.00018540227,0.00047439098],"category_scores_gemma":[0.00030560902,0.00011085615,0.00010270177,0.00077489094,0.0002003727,0.00018991016,0.00023425797,0.00021142767,0.0000772891],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00049014646,0.00008027916,0.74997026,0.000062207204,0.000060552073,0.00032101912,0.00088358554,0.0027025123,0.21967158,0.00011460844,0.00074544817,0.024897791],"study_design_scores_gemma":[0.0000056069775,0.0000450748,0.9857824,0.0000044383874,0.000016951673,0.000051956184,0.0003118061,0.004238903,0.009074274,0.000019379868,0.00043652346,0.000012674381],"about_ca_topic_score_codex":0.099269204,"about_ca_topic_score_gemma":0.23001292,"teacher_disagreement_score":0.099269204,"about_ca_system_score_codex":0.0006247724,"about_ca_system_score_gemma":0.0006354804,"threshold_uncertainty_score":0.19738281},"labels":[],"label_agreement":null},{"id":"W2607010739","doi":"10.1002/2016jb013601","title":"Formation of a solid inner core during the accretion of Earth","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Inner core; Accretion (finance); Core (optical fiber); RADIUS; Adiabatic process; Earth (classical element); Thermal; Outer core; Geology; Physics; Mechanics; Astrophysics; Geophysics; Thermodynamics; Astronomy","score_opus":0.06288823317952857,"score_gpt":0.35377420845347257,"score_spread":0.290885975273944,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2607010739","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99652004,0.000038238508,0.0017979017,0.000008476308,0.0000032357275,0.00000778514,0.000035614514,0.000028558125,0.0015602917],"genre_scores_gemma":[0.9992137,0.000017903143,0.00041505686,0.0000025039978,9.0007075e-7,0.0000031559964,0.00005027227,0.0000088191,0.00028755717],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999064,0.000014973075,0.00000465475,0.00001681052,0.000026122947,0.00003107009],"domain_scores_gemma":[0.9997801,0.00005376774,0.00005943622,0.00003513878,0.000027804484,0.000043779444],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019038717,0.0003610061,0.00038372594,0.00031988966,0.0004087053,0.0006989161,0.0004570869,0.00033933754,0.000728538],"category_scores_gemma":[0.0005609612,0.00026573832,0.00047016604,0.00016767449,0.0005118396,0.00036105924,0.0005506675,0.00025676226,0.00012160287],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035424082,0.000110484354,0.027453728,0.00008100356,0.000088794295,0.000682392,0.00023371167,0.8818199,0.07995369,0.004024894,0.0001965452,0.0050005205],"study_design_scores_gemma":[0.000053472137,0.00030119455,0.015857179,0.000011606609,0.000032404234,0.00021587283,0.000084618885,0.95715755,0.024858218,0.0006673047,0.0007417711,0.00001886337],"about_ca_topic_score_codex":0.004213491,"about_ca_topic_score_gemma":0.0016704465,"teacher_disagreement_score":0.004213491,"about_ca_system_score_codex":0.000633785,"about_ca_system_score_gemma":0.00032406492,"threshold_uncertainty_score":0.00837791},"labels":[],"label_agreement":null},{"id":"W2607617830","doi":"10.1002/2016jb013599","title":"Seismic anisotropy of Precambrian lithosphere: Insights from Rayleigh wave tomography of the eastern Superior Craton","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"National Science Foundation","keywords":"Lithosphere; Geology; Craton; Archean; Precambrian; Proterozoic; Seismic anisotropy; Tectonics; Seismology; Geophysics; Plate tectonics; Paleontology; Mantle (geology)","score_opus":0.0325607555067306,"score_gpt":0.28620392599211797,"score_spread":0.25364317048538737,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2607617830","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973858,0.00012284935,0.0004345944,0.000046966285,0.000002007061,0.000009055695,0.00044531142,0.00004843258,0.0015048846],"genre_scores_gemma":[0.9989641,0.0001028474,0.00039525126,0.000007155314,0.0000021485214,0.0000019259626,0.00025402423,0.000008022993,0.00026458516],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999509,0.000002181106,0.0000021732244,0.000008927647,0.00001917232,0.000016710837],"domain_scores_gemma":[0.99988055,0.000014128914,0.000021282834,0.0000102410295,0.000050636638,0.00002311938],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000097480224,0.00037835195,0.00020254559,0.0013495089,0.0003062203,0.00056042895,0.00030173562,0.00022848032,0.0010180513],"category_scores_gemma":[0.00038003776,0.00023576888,0.00016585145,0.001292474,0.00037167588,0.00017405124,0.00032453611,0.0001737266,0.0001718625],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042335477,0.00009237161,0.720122,0.00015996359,0.0001822408,0.002112302,0.0017606025,0.036122464,0.19754478,0.0011647699,0.0012677747,0.0390474],"study_design_scores_gemma":[0.000012138914,0.000016198119,0.9768141,0.000015026055,0.000027268106,0.00016540528,0.00032481377,0.019780606,0.0020652858,0.00008690756,0.00067970617,0.000012590277],"about_ca_topic_score_codex":0.43686166,"about_ca_topic_score_gemma":0.5357803,"teacher_disagreement_score":0.43686166,"about_ca_system_score_codex":0.00087451265,"about_ca_system_score_gemma":0.0015410887,"threshold_uncertainty_score":0.8686377},"labels":[],"label_agreement":null},{"id":"W2608290825","doi":"10.1002/2016jb013744","title":"The thermo‐hydro‐mechanical behavior of the argillaceous Cobourg Limestone","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Rock Mechanics and Modeling","field":"Engineering","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Sedimentary rock; Geology; Biot number; Calcite; Dolomite; Pore water pressure; Permeability (electromagnetism); Mineralogy; Paleozoic; Geotechnical engineering; Petrology; Geochemistry; Mechanics","score_opus":0.0453082380808598,"score_gpt":0.3433246133665839,"score_spread":0.29801637528572406,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2608290825","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99969494,0.0000140885395,0.00003569774,0.0000022837237,3.829724e-7,0.0000031552318,0.00002445147,0.0000027032947,0.00022226098],"genre_scores_gemma":[0.999678,0.000009063212,0.00007773732,0.0000020640014,2.8563696e-7,0.00000270195,0.00002963859,0.0000014556535,0.00019916093],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999211,0.000004857521,0.0000026839853,0.00002650224,0.000025831248,0.00001896998],"domain_scores_gemma":[0.9998764,0.000030992625,0.000022744902,0.000013557041,0.000033551503,0.0000228159],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013652924,0.0001833797,0.00022566279,0.00038033968,0.0003776444,0.00031852417,0.0002655871,0.00022466341,0.0008717323],"category_scores_gemma":[0.00027938135,0.00014531436,0.00009013364,0.00023698952,0.00083880866,0.00014569341,0.00018080797,0.00014824557,0.000099301855],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00053776026,0.000050788396,0.04510735,0.000064714426,0.0000148751205,0.00047091208,0.00052918884,0.0025363571,0.9463103,0.0001432153,0.000057440742,0.004177104],"study_design_scores_gemma":[0.000033894554,0.0004731364,0.78057,0.000010763232,0.00001694596,0.00026209213,0.0009766531,0.0070977034,0.2091976,0.000058475252,0.0012819865,0.000020885414],"about_ca_topic_score_codex":0.044506084,"about_ca_topic_score_gemma":0.066085674,"teacher_disagreement_score":0.044506084,"about_ca_system_score_codex":0.00073640747,"about_ca_system_score_gemma":0.0002905329,"threshold_uncertainty_score":0.08849406},"labels":[],"label_agreement":null},{"id":"W2608712298","doi":"10.1029/2017jb014671","title":"A Broadband Laboratory Study of the Seismic Properties of Cracked and Fluid‐Saturated Synthetic Glass Media","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Lawrence Berkeley National Laboratory; Basic Energy Sciences; Australian Research Council; Office of Science; University of Alberta; U.S. Department of Energy","keywords":"Materials science; Saturation (graph theory); Shear modulus; Composite material; Bulk modulus; Ultrasonic sensor; Porous medium; Porosity; Elastic modulus; Mineralogy; Shear waves; Shear (geology); Geology; Acoustics","score_opus":0.034990596779717754,"score_gpt":0.28501500184424644,"score_spread":0.25002440506452867,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2608712298","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976476,0.00007419297,0.0018271384,0.000010068984,0.0000025763068,0.000006255988,0.00008584042,0.000029814813,0.00031652118],"genre_scores_gemma":[0.998553,0.000058096724,0.0010307131,0.0000065627823,0.0000026924179,0.000010622663,0.000096756936,0.000006097883,0.00023532742],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.999889,0.000013718329,0.000007041006,0.000025767853,0.000043889104,0.000020637808],"domain_scores_gemma":[0.99974793,0.0000665035,0.0000834849,0.00002576353,0.0000481098,0.000028270319],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015807134,0.00028142327,0.00014613711,0.00024569442,0.00015606805,0.00016962136,0.00017473917,0.0002030706,0.00083611504],"category_scores_gemma":[0.00032439255,0.00013987621,0.000102333215,0.00015566172,0.0003245497,0.0001738101,0.00024703259,0.00018132989,0.00012035847],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002531808,0.0000064507467,0.00042185356,0.00001137403,0.0000017592089,0.000016697022,0.000020020936,0.00008365998,0.99894613,0.000023208573,0.0000061767205,0.00043737088],"study_design_scores_gemma":[0.000006529367,0.000530276,0.008722029,0.000004627834,0.000010166046,0.00009123702,0.00008233976,0.0021648612,0.98799056,0.000025926554,0.00036344887,0.000008062539],"about_ca_topic_score_codex":0.0007157343,"about_ca_topic_score_gemma":0.0008083862,"teacher_disagreement_score":0.00083611504,"about_ca_system_score_codex":0.00014320783,"about_ca_system_score_gemma":0.00009632196,"threshold_uncertainty_score":0.0027970672},"labels":[],"label_agreement":null},{"id":"W2608940261","doi":"10.1002/2016jb013503","title":"Physical mechanisms for multiphase flow associated with hydrate formation","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Department of Mechanical Engineering, University of Texas at Austin; U.S. Department of Energy","keywords":"Clathrate hydrate; Hydrate; Saturation (graph theory); Geology; Capillary pressure; Methane; Petrology; Mineralogy; Geotechnical engineering; Chemistry; Porous medium; Porosity","score_opus":0.04216432209906332,"score_gpt":0.34288940563525316,"score_spread":0.3007250835361899,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2608940261","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9840947,0.0003589372,0.013227748,0.00024389787,0.000026693413,0.00003761246,0.000090793495,0.00014760644,0.0017719319],"genre_scores_gemma":[0.9992199,0.00007000569,0.00044418956,0.000006829319,0.0000035551482,0.000008774022,0.000020618843,0.0000019178715,0.00022412164],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99995124,0.000006326325,0.0000033978672,0.000014443325,0.000010540753,0.000014040692],"domain_scores_gemma":[0.9998735,0.00003189332,0.000042074702,0.000012384659,0.000019209489,0.00002088693],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001893251,0.00026309103,0.0002231826,0.0005117752,0.0005074585,0.000496744,0.00046571647,0.00053485984,0.0013728956],"category_scores_gemma":[0.00027544607,0.00033609985,0.00035198548,0.00013495043,0.00066753867,0.0006855629,0.0004919429,0.00028950322,0.00012406496],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042577818,0.00027846202,0.06662819,0.00036487085,0.00010387687,0.0019393277,0.0005037537,0.24600539,0.62588185,0.046310022,0.0008776167,0.010680833],"study_design_scores_gemma":[0.000072439754,0.00025143387,0.044406738,0.000023092669,0.000037730497,0.0003803522,0.00031364366,0.8618744,0.078502245,0.012283277,0.0017901326,0.00006450524],"about_ca_topic_score_codex":0.003900295,"about_ca_topic_score_gemma":0.0015090859,"teacher_disagreement_score":0.003900295,"about_ca_system_score_codex":0.0009466111,"about_ca_system_score_gemma":0.00041554647,"threshold_uncertainty_score":0.0077551603},"labels":[],"label_agreement":null},{"id":"W2617323716","doi":"10.1002/2017jb014924","title":"Changes in Physical Properties of the Nankai Trough Megasplay Fault Induced by Earthquakes, Detected by Continuous Pressure Monitoring","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismology and Earthquake Studies","field":"Computer Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Geomechanica (Canada)","funders":"National Research Institute for Earth Science and Disaster Prevention; Deutsche Forschungsgemeinschaft; National Science Foundation","keywords":"Seismology; Geology; Trough (economics); San andreas fault; Fault (geology)","score_opus":0.043315339265019036,"score_gpt":0.3174379884902579,"score_spread":0.2741226492252389,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2617323716","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99960965,0.000012207352,0.00010692146,0.0000053042777,0.0000010061657,0.0000023415746,0.00013697914,0.00000660208,0.00011908391],"genre_scores_gemma":[0.9996635,0.000010486731,0.00009168432,0.0000022562824,0.0000016849663,0.0000029471958,0.00017705612,8.8954033e-7,0.000049517792],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999435,0.000005307254,0.0000054405364,0.000017853316,0.000016937372,0.000010881389],"domain_scores_gemma":[0.9997614,0.000031573152,0.00010456305,0.000019478573,0.000042791788,0.000040184677],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012575352,0.00018591441,0.00015333589,0.00058608653,0.00015520863,0.0002269531,0.00017427077,0.00022082627,0.00044700684],"category_scores_gemma":[0.00044090414,0.000115947645,0.00010707936,0.00050380215,0.00017473966,0.00022658489,0.00022440267,0.00013324125,0.0000767596],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018059845,0.000089725065,0.9278451,0.00003178557,0.000059258742,0.0003048996,0.00021219107,0.0022781664,0.057004865,0.000044694603,0.00020472215,0.01174404],"study_design_scores_gemma":[0.0000017443583,0.00002278439,0.99727446,8.1201705e-7,0.000005195177,0.000024538396,0.000034913264,0.0019614205,0.0006259666,0.000005848162,0.00004020907,0.0000020516884],"about_ca_topic_score_codex":0.0063903276,"about_ca_topic_score_gemma":0.009020155,"teacher_disagreement_score":0.0063903276,"about_ca_system_score_codex":0.00020243437,"about_ca_system_score_gemma":0.0001447642,"threshold_uncertainty_score":0.01270628},"labels":[],"label_agreement":null},{"id":"W2619150855","doi":"10.1002/2016jb013785","title":"Constraints on melt content of off‐axis magma lenses at the East Pacific Rise from analysis of 3‐D seismic amplitude variation with angle of incidence","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"BP (Canada); Shell (Canada); Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Courant Forschungszentrum Geobiologie, Georg-August-Universität Göttingen; Canada Foundation for Innovation; National Science Foundation","keywords":"Geology; Mantle (geology); Amplitude; Magma; Magma chamber; Mineralogy; Partial melting; Seismology; Petrology; Geochemistry; Volcano; Optics","score_opus":0.05882623067232355,"score_gpt":0.30742997354940327,"score_spread":0.2486037428770797,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2619150855","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988814,0.00003083099,0.0003891369,0.0000046982886,6.886468e-7,0.000002526862,0.00018227837,0.000019076095,0.00048933306],"genre_scores_gemma":[0.99910957,0.00002941988,0.00050641934,0.0000019641186,0.0000015495965,0.0000027548328,0.00027150323,0.000009020705,0.000067714944],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999012,0.000008354513,0.0000069906228,0.00002599775,0.000035468893,0.000021965601],"domain_scores_gemma":[0.9997259,0.000068275374,0.000088318426,0.000019394542,0.00005833584,0.000039870047],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016193568,0.0002933513,0.00020296237,0.0015083338,0.00026364648,0.0007606702,0.00017793896,0.00015062989,0.00073552306],"category_scores_gemma":[0.00055044395,0.00019910393,0.00027907788,0.0009436655,0.00027737618,0.0002689104,0.00042703975,0.0001755461,0.00010064632],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020932723,0.00002522582,0.87185645,0.00003745997,0.00008043123,0.00019164155,0.00053419435,0.0015719829,0.10684818,0.0000980231,0.00010092589,0.018446112],"study_design_scores_gemma":[0.000001247854,0.000007094794,0.9964277,0.0000019763822,0.00001037635,0.000024279341,0.000099249744,0.0014353723,0.0018591464,0.000012554859,0.00011810073,0.000002940936],"about_ca_topic_score_codex":0.027095456,"about_ca_topic_score_gemma":0.05084672,"teacher_disagreement_score":0.027095456,"about_ca_system_score_codex":0.00031017195,"about_ca_system_score_gemma":0.0002426309,"threshold_uncertainty_score":0.053875506},"labels":[],"label_agreement":null},{"id":"W2619414478","doi":"10.1002/2017jb014248","title":"Slip Behavior of the Queen Charlotte Plate Boundary Before and After the 2012, <i>M</i><sub><i>W</i></sub> 7.8 Haida Gwaii Earthquake: Evidence From Repeating Earthquakes","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Seismology; Geology; Subduction; Episodic tremor and slip; Slip (aerodynamics); Plate tectonics; Interplate earthquake; Thrust fault; Seismic hazard; Fault (geology); Tectonics; Engineering","score_opus":0.03465619226459602,"score_gpt":0.30047934055118847,"score_spread":0.2658231482865924,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2619414478","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992392,0.000014920548,0.000015637228,0.000005745689,8.6955333e-7,0.0000031162392,0.0001938171,0.0000031277586,0.0005236337],"genre_scores_gemma":[0.9989668,0.000022504923,0.000050539395,0.0000042056777,0.0000013242338,0.0000051847132,0.0005494081,0.0000017547379,0.00039821962],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999101,0.0000069959206,0.00000567246,0.000023805069,0.000031246647,0.000022156642],"domain_scores_gemma":[0.99935585,0.00004489079,0.00022793816,0.000033908233,0.00017100295,0.00016643583],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013967163,0.00013940233,0.00025669593,0.001371957,0.00048299425,0.0005804913,0.0002391682,0.00024378428,0.0009864894],"category_scores_gemma":[0.0007716391,0.00017072995,0.00008198794,0.0012505852,0.0004135372,0.00018469103,0.0004142553,0.0001514108,0.00039550412],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014449442,0.00003144144,0.9854079,0.000017945538,0.0000202614,0.00034640828,0.0011230846,0.0005130764,0.0056961044,0.000035876343,0.00044384977,0.006219629],"study_design_scores_gemma":[0.0000010836774,0.000008290278,0.99945575,0.0000020668633,0.0000012481642,0.000020620506,0.00015013409,0.00017432343,0.000095179,0.0000025372253,0.000087298016,0.0000015059195],"about_ca_topic_score_codex":0.12726489,"about_ca_topic_score_gemma":0.26483414,"teacher_disagreement_score":0.87273514,"about_ca_system_score_codex":0.00094021164,"about_ca_system_score_gemma":0.0005302123,"threshold_uncertainty_score":0.25304824},"labels":[],"label_agreement":null},{"id":"W2623708897","doi":"10.1002/2016jb013865","title":"Upper crustal investigation of the Gulf of Saint Lawrence region, eastern Canada using ambient noise tomography","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Laurentia; Terrane; Geology; Crust; Craton; Proterozoic; Fibrous joint; Lithosphere; Paleontology; Seismology; Basement; Structural basin; Archean; Anorthosite; Tectonics; Geography; Archaeology","score_opus":0.0511391370402156,"score_gpt":0.2941175874562552,"score_spread":0.2429784504160396,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2623708897","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958288,0.0001270885,0.0001865623,0.000052350813,0.0000022923427,0.000009609025,0.0010738111,0.000029007859,0.0026904456],"genre_scores_gemma":[0.9971968,0.000147911,0.0005433147,0.000020486184,0.0000016725417,0.00000435907,0.00077150733,0.000005556926,0.0013083462],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998832,0.000003586908,0.0000046761224,0.000018267212,0.000056188303,0.000034143788],"domain_scores_gemma":[0.9997589,0.0000078338,0.000024426465,0.000006521801,0.00017296916,0.000029371415],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009771894,0.0002349451,0.00013375592,0.001182407,0.0010935788,0.00077406067,0.00036573503,0.00016418984,0.00064496906],"category_scores_gemma":[0.0002499276,0.00014628014,0.00014546742,0.0016250071,0.00029441656,0.00015853505,0.00038290612,0.0001715884,0.0001413744],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007389593,0.00002668023,0.95750016,0.000049204606,0.000058064896,0.0006431539,0.0011958345,0.0027335293,0.013011951,0.00038301805,0.00083268376,0.023491858],"study_design_scores_gemma":[0.000005067266,0.000008184477,0.99280566,0.000015683316,0.000014108558,0.000053774587,0.00094556843,0.0027129368,0.000847303,0.0000306394,0.0025518104,0.000009358257],"about_ca_topic_score_codex":0.98138773,"about_ca_topic_score_gemma":0.9934847,"teacher_disagreement_score":0.018612266,"about_ca_system_score_codex":0.0061755,"about_ca_system_score_gemma":0.0072755404,"threshold_uncertainty_score":0.0448066},"labels":[],"label_agreement":null},{"id":"W2625175538","doi":"10.1002/2016jb013789","title":"The effect of speleothem surface slope on the remanent magnetic inclination","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Fundação para a Ciência e a Tecnologia; Universidade de Lisboa; Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Speleothem; Geology; Calcite; Paleomagnetism; Remanence; Natural remanent magnetization; Rock magnetism; Anisotropy; Magnetic mineralogy; Geophysics; Magnetization; Paleontology; Magnetic field; Physics; Cave; Geography","score_opus":0.03694665614014978,"score_gpt":0.3450358002764989,"score_spread":0.3080891441363491,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2625175538","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988839,0.000080949794,0.00017857093,0.0000045215356,0.0000012832269,0.0000012491143,0.00020363237,0.000013406684,0.0006323968],"genre_scores_gemma":[0.9997286,0.000024022238,0.000057718145,0.0000018482634,8.925386e-7,7.680118e-7,0.000119188866,0.000004723218,0.00006231364],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998926,0.000021139831,0.000007853212,0.00003459341,0.000022777594,0.000021078913],"domain_scores_gemma":[0.9996131,0.00015469821,0.000085141284,0.000050860162,0.000053052703,0.000043216853],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015629396,0.0001920769,0.0002245949,0.00047409377,0.00022845287,0.000577347,0.0001712636,0.00020355133,0.0010237957],"category_scores_gemma":[0.00064290146,0.00020292483,0.00018765799,0.0003714387,0.0002800534,0.00014819385,0.0002073081,0.00012525197,0.00025228126],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026668407,0.00001293071,0.75928396,0.00006929397,0.000110913876,0.00022955539,0.0002458977,0.0010854137,0.23067759,0.0000512829,0.00009175181,0.007874721],"study_design_scores_gemma":[7.7078084e-7,0.000010349249,0.9973363,0.000002317461,0.0000054802404,0.000048712875,0.000031245207,0.00031610756,0.002146092,0.000007179169,0.00009385955,0.0000015612204],"about_ca_topic_score_codex":0.0032099367,"about_ca_topic_score_gemma":0.0061504524,"teacher_disagreement_score":0.0032099367,"about_ca_system_score_codex":0.00019385034,"about_ca_system_score_gemma":0.00011819952,"threshold_uncertainty_score":0.006382525},"labels":[],"label_agreement":null},{"id":"W2661761461","doi":"10.1002/2017jb014284","title":"Architecture of the crust and uppermost mantle in the northern Canadian Cordillera from receiver functions","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada; Ontario Ministry of Research, Innovation and Science; Agence Nationale de la Recherche; National Science Foundation","keywords":"Geology; Crust; Seismology; Mantle (geology); Lithosphere; Anisotropy; Receiver function; Seismic anisotropy; Crustal recycling; Geophysics; Tectonics; Continental crust; Petrology","score_opus":0.029057416687403113,"score_gpt":0.2816063291608422,"score_spread":0.2525489124734391,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2661761461","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9917236,0.00023456491,0.0032467626,0.00008078401,0.0000037197483,0.000009642176,0.00060397835,0.0002145011,0.0038825057],"genre_scores_gemma":[0.9976981,0.000059894508,0.0012244814,0.0000058017404,0.0000014232076,0.0000021218393,0.00034104218,0.00001448502,0.00065263454],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999201,0.000004939486,0.0000024274277,0.000017872402,0.000029630759,0.000024969526],"domain_scores_gemma":[0.99989605,0.000014783528,0.000015957266,0.0000052465894,0.00005607073,0.000011960312],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013579386,0.0006430221,0.00016536714,0.0009810588,0.000669899,0.0008550724,0.0006576596,0.0003272581,0.0022711763],"category_scores_gemma":[0.00052221835,0.00024855905,0.00029946014,0.0012767604,0.00030599383,0.00023513626,0.00024495434,0.00016276713,0.00019872424],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024821985,0.00006247802,0.30551204,0.00014048978,0.00017976254,0.00061492564,0.00057895505,0.52033263,0.08091098,0.0056394073,0.001503989,0.08427604],"study_design_scores_gemma":[0.0000268783,0.000025192341,0.466502,0.0000291278,0.000082718936,0.000088855995,0.00018611841,0.524353,0.005928953,0.0007901076,0.0019297751,0.000057183697],"about_ca_topic_score_codex":0.9003126,"about_ca_topic_score_gemma":0.86177117,"teacher_disagreement_score":0.0996874,"about_ca_system_score_codex":0.0055448506,"about_ca_system_score_gemma":0.0034089277,"threshold_uncertainty_score":0.20054889},"labels":[],"label_agreement":null},{"id":"W2670729628","doi":"10.1002/2017jb014368","title":"Source model for the Copahue volcano magma plumbing system constrained by InSAR surface deformation observations","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Geology; Interferometric synthetic aperture radar; Seismology; Induced seismicity; Caldera; Volcano; Fault (geology); Geodesy; Synthetic aperture radar; Remote sensing","score_opus":0.07699275052855369,"score_gpt":0.3032537440293687,"score_spread":0.22626099350081502,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2670729628","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95712936,0.00030676802,0.020209383,0.00040723264,0.0000556461,0.00007595866,0.012826261,0.0009817865,0.008007512],"genre_scores_gemma":[0.9902222,0.00007110745,0.0021395325,0.000032123466,0.000018616192,0.000045245135,0.005978898,0.00006403483,0.0014282027],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99988854,0.000014902632,0.000007166404,0.0000485775,0.000015834707,0.000024909443],"domain_scores_gemma":[0.9997867,0.00006158237,0.00003944182,0.000039086615,0.000050032704,0.000023165254],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020639354,0.0006160476,0.00046380394,0.0008059623,0.0003694364,0.00093055714,0.0009871908,0.0009580791,0.00404565],"category_scores_gemma":[0.00075352227,0.00047673192,0.00070879207,0.00073475175,0.00030662844,0.0005781777,0.000408422,0.00057119376,0.000819465],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009026403,0.00006239035,0.038817916,0.000040138548,0.00011460216,0.00022549626,0.000052780753,0.94967604,0.0020182873,0.00163883,0.0022223117,0.005040909],"study_design_scores_gemma":[0.000026277507,0.000011291537,0.010835746,0.0000053926456,0.000014254726,0.000040565086,0.000023225384,0.9870974,0.00031039293,0.0005165621,0.0011052972,0.000013528358],"about_ca_topic_score_codex":0.09290123,"about_ca_topic_score_gemma":0.051070407,"teacher_disagreement_score":0.09290123,"about_ca_system_score_codex":0.0009648739,"about_ca_system_score_gemma":0.0009389016,"threshold_uncertainty_score":0.184721},"labels":[],"label_agreement":null},{"id":"W2725585300","doi":"10.1002/2017jb014035","title":"Large and primarily updip afterslip following the 2012 <i>M</i><sub><i>w</i></sub> 7.6 Nicoya, Costa Rica, earthquake","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Division of Earth Sciences; National Science Foundation of Sri Lanka; Natural Sciences and Engineering Research Council of Canada; College of Computing; National Science Foundation","keywords":"Geology; Seismology; Slip (aerodynamics); Moment magnitude scale; Geodesy; Aftershock; Geometry; Physics","score_opus":0.03253951993068241,"score_gpt":0.30651117599316546,"score_spread":0.2739716560624831,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2725585300","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976647,0.000044650067,0.00013580701,0.000027736605,0.000004258827,0.0000072069874,0.00047782695,0.000031195876,0.0016064753],"genre_scores_gemma":[0.9990103,0.000030586343,0.00008682896,0.000011328966,0.0000047812478,0.000006012857,0.00048447313,0.000004025907,0.00036173157],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999261,0.0000057014468,0.000004225616,0.000016293854,0.000022088429,0.000025637984],"domain_scores_gemma":[0.99983513,0.000010212447,0.000064142296,0.000020289066,0.000046956517,0.000023204166],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000812113,0.00018182333,0.00019021753,0.00040087508,0.00028747364,0.00036764052,0.00020202347,0.00022533597,0.0007432742],"category_scores_gemma":[0.00028364366,0.000113861504,0.00013034404,0.0003961605,0.00018231844,0.00012657193,0.0003228219,0.00020293491,0.00015063504],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000182224,0.00007432782,0.93734545,0.000056708337,0.00010189634,0.0005878794,0.00047164128,0.0025841792,0.037116386,0.00014066805,0.0016609154,0.019677801],"study_design_scores_gemma":[9.544693e-7,0.0000087064,0.9988047,0.0000023777534,0.0000036903589,0.00002174802,0.00005990527,0.00040013817,0.00038517313,0.0000035311814,0.00030743054,0.0000016985132],"about_ca_topic_score_codex":0.04642305,"about_ca_topic_score_gemma":0.11449955,"teacher_disagreement_score":0.04642305,"about_ca_system_score_codex":0.00051421917,"about_ca_system_score_gemma":0.00028643294,"threshold_uncertainty_score":0.09230566},"labels":[],"label_agreement":null},{"id":"W2726667971","doi":"10.1002/2017jb014261","title":"Absolute reconstruction of the closing of the Mongol‐Okhotsk Ocean in the Mesozoic elucidates the genesis of the slab geometry underneath Eurasia","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Lithosphere; Mantle (geology); Subduction; Convergent boundary; Fibrous joint; Paleontology; Paleomagnetism; Mesozoic; Stage (stratigraphy); Oceanic crust; Tectonics; Structural basin","score_opus":0.041839667581095204,"score_gpt":0.30977616861814083,"score_spread":0.26793650103704564,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2726667971","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9950507,0.00032665214,0.0024268012,0.000065303575,0.000014904144,0.0000037462564,0.00030546502,0.00007109481,0.0017353294],"genre_scores_gemma":[0.99897873,0.00005105744,0.0005481154,0.000004749167,0.0000019759166,0.000001420138,0.00020933348,0.000010957929,0.00019358096],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999869,0.000019302322,0.000012422977,0.000050025606,0.000022749984,0.000026525386],"domain_scores_gemma":[0.9998159,0.000015566491,0.00004653354,0.000041357802,0.000052756568,0.000027924052],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038938032,0.00029793603,0.00023324725,0.0011085791,0.0005028987,0.0010091715,0.00041958928,0.0004219633,0.0020538804],"category_scores_gemma":[0.0009621406,0.00031940025,0.0004693224,0.0008221364,0.00051808346,0.00040155547,0.0007861512,0.00046143756,0.00026545874],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046731974,0.00004514656,0.77700305,0.00020677753,0.0005639476,0.0006363514,0.0024182007,0.06394125,0.08367326,0.0068258652,0.00062236807,0.063596494],"study_design_scores_gemma":[0.00001878292,0.00003849193,0.96574193,0.000031518593,0.00006775235,0.00016657979,0.0004684787,0.028100327,0.0027088167,0.0004346022,0.0021965657,0.000026203144],"about_ca_topic_score_codex":0.03060566,"about_ca_topic_score_gemma":0.03675297,"teacher_disagreement_score":0.03060566,"about_ca_system_score_codex":0.00067967933,"about_ca_system_score_gemma":0.00083721563,"threshold_uncertainty_score":0.06085503},"labels":[],"label_agreement":null},{"id":"W2731031470","doi":"10.1002/2017jb014259","title":"Constant electrical resistivity of Ni along the melting boundary up to 9 GPa","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Foundation for Innovation","keywords":"Electrical resistivity and conductivity; Condensed matter physics; Materials science; Thermodynamics; Fermi liquid theory; Mineralogy; Analytical Chemistry (journal); Chemistry; Superconductivity; Physics","score_opus":0.047081064033482285,"score_gpt":0.34383908644732436,"score_spread":0.2967580224138421,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2731031470","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9907004,0.00025587986,0.0021829854,0.00017053566,0.000012444967,0.000008242583,0.0005571528,0.00024659385,0.005865866],"genre_scores_gemma":[0.99895453,0.00004730369,0.00034329906,0.000007953151,0.0000033459164,0.000006218198,0.00023650604,0.000013322159,0.0003875458],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99988294,0.000009747444,0.000004615996,0.000029384923,0.00005005599,0.00002314911],"domain_scores_gemma":[0.9998246,0.00004044937,0.000035568064,0.000023884528,0.000059632304,0.000015982137],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008965454,0.00016964952,0.00020427267,0.00034929588,0.0003806783,0.0004316023,0.00037917285,0.00030779294,0.0013204255],"category_scores_gemma":[0.00045926738,0.00018002269,0.00008957438,0.00033269718,0.0005729721,0.0007051055,0.00043586505,0.0006180901,0.00042053717],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030931397,0.00003451379,0.009642479,0.00011978585,0.000016656402,0.0004993686,0.0004200482,0.0014870402,0.9777104,0.0019501677,0.000664983,0.007145261],"study_design_scores_gemma":[0.000021926537,0.00031019136,0.062309865,0.000032643784,0.000017402548,0.0004953559,0.00044356927,0.016595408,0.9108273,0.0020611507,0.006861247,0.0000239972],"about_ca_topic_score_codex":0.00113661,"about_ca_topic_score_gemma":0.0006922438,"teacher_disagreement_score":0.0013204255,"about_ca_system_score_codex":0.00021060013,"about_ca_system_score_gemma":0.00013709908,"threshold_uncertainty_score":0.0044172406},"labels":[],"label_agreement":null},{"id":"W2732019400","doi":"10.1002/2016jb013828","title":"Grain size‐dependent strength of phyllosilicate‐rich gouges in the shallow crust: Insights from the SAFOD site","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; University of New Brunswick","funders":"","keywords":"Geology; Brittleness; Grain size; Creep; Quartz; Pressure solution; Deformation (meteorology); Fault gouge; Mineralogy; Slip (aerodynamics); Strain rate; Diffusion creep; Petrology; Fault (geology); Seismology; Composite material; Diagenesis; Materials science; Grain boundary; Geomorphology; Microstructure","score_opus":0.04733484949062085,"score_gpt":0.32450157419461756,"score_spread":0.2771667247039967,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2732019400","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99943894,0.000052164152,0.000046597073,0.000012453164,7.472768e-7,0.0000017905344,0.00013989037,0.0000061667865,0.00030130395],"genre_scores_gemma":[0.9995758,0.00004071568,0.0000771433,0.000009119193,0.000001385825,0.0000014313836,0.00013805131,0.000004276918,0.00015199874],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999114,0.0000056205354,0.000006632001,0.000035910638,0.0000223021,0.00001803377],"domain_scores_gemma":[0.9997961,0.000022881351,0.00006242271,0.000013697889,0.000054945136,0.000049890135],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016765163,0.00027861155,0.0003564563,0.0012957397,0.00041875898,0.0004951939,0.00031327907,0.00037095623,0.0013365512],"category_scores_gemma":[0.0003644078,0.0002922411,0.00018485454,0.00059448194,0.00050109735,0.00031008918,0.00047284135,0.00017508274,0.00029817782],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001448325,0.000044565775,0.89898556,0.00006341284,0.000070985225,0.0003401492,0.00086300704,0.0006735231,0.09408638,0.000087205226,0.00010777182,0.0045325793],"study_design_scores_gemma":[0.0000030174904,0.000018092393,0.9980386,0.0000029292742,0.0000073490546,0.000057288584,0.00020810925,0.00040351652,0.001050384,0.00001776409,0.00018921206,0.0000037946181],"about_ca_topic_score_codex":0.029673003,"about_ca_topic_score_gemma":0.071279645,"teacher_disagreement_score":0.029673003,"about_ca_system_score_codex":0.00057607394,"about_ca_system_score_gemma":0.00021323595,"threshold_uncertainty_score":0.05900061},"labels":[],"label_agreement":null},{"id":"W2735575745","doi":"10.1002/2017jb014150","title":"Detailed crustal thickness variations beneath the Illinois Basin area: Implications for crustal evolution of the midcontinent","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"University of Illinois at Urbana-Champaign; Lilly Endowment; Purdue University; Eli Lilly and Company; National Science Foundation","keywords":"Geology; Crust; Precambrian; Underplating; Rift; Proterozoic; Structural basin; Seismology; Paleontology; Subduction; Tectonics; Geomorphology","score_opus":0.048795533543013636,"score_gpt":0.3242039333479002,"score_spread":0.27540839980488657,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2735575745","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979652,0.00012461947,0.00012897568,0.000043030137,8.5803566e-7,0.0000022516163,0.00015498437,0.000016766686,0.001563352],"genre_scores_gemma":[0.99945575,0.00005097767,0.00013705959,0.000009119551,9.842917e-7,0.0000022813401,0.00010482668,0.0000025202742,0.0002365243],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995005,0.0000070435644,0.0000024203182,0.00001554422,0.000010256901,0.000014721295],"domain_scores_gemma":[0.99980336,0.00003319559,0.000049842416,0.000013625003,0.000060352424,0.00003973166],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016001199,0.00014669598,0.00008887712,0.0015008801,0.00037358294,0.0007482772,0.00019651308,0.00018727474,0.0017499935],"category_scores_gemma":[0.00033286092,0.00013473762,0.000111072004,0.000684068,0.00041826643,0.00025705766,0.00046536405,0.00011911895,0.00013164044],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000060966733,0.000010632102,0.97601366,0.000013400829,0.000033697906,0.00012501274,0.00048243444,0.0015064063,0.01291431,0.00017942033,0.00016018095,0.008499952],"study_design_scores_gemma":[7.037537e-7,0.0000023623759,0.999151,0.0000042819834,0.0000027326819,0.000012454648,0.00011312806,0.00036022483,0.00016247293,0.000019467348,0.00016925734,0.0000018505139],"about_ca_topic_score_codex":0.07054826,"about_ca_topic_score_gemma":0.15509674,"teacher_disagreement_score":0.07054826,"about_ca_system_score_codex":0.0008188311,"about_ca_system_score_gemma":0.0003083287,"threshold_uncertainty_score":0.14027524},"labels":[],"label_agreement":null},{"id":"W2737206241","doi":"10.1002/2017jb013979","title":"Modeling of viscoelastic properties of nonpermeable porous rocks saturated with highly viscous fluid at seismic frequencies at the core scale","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"China Postdoctoral Science Foundation; National Natural Science Foundation of China","keywords":"Viscoelasticity; Viscosity; Porous medium; Poromechanics; Porosity; Materials science; Dispersion (optics); Elastic modulus; Volume viscosity; Mechanics; Geotechnical engineering; Geology; Mineralogy; Composite material; Physics; Optics","score_opus":0.05199251383947507,"score_gpt":0.2860916535276985,"score_spread":0.23409913968822343,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2737206241","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.85555,0.000116498995,0.14126961,0.00008438237,0.000009929621,0.000028141907,0.00008257172,0.00019414435,0.0026647376],"genre_scores_gemma":[0.99525815,0.000053295593,0.004088482,0.0000056698973,0.0000028223683,0.000018171933,0.000028792798,0.000011224631,0.0005332684],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992716,0.000013857392,0.000005438227,0.000014478516,0.000026365364,0.000012698299],"domain_scores_gemma":[0.99978834,0.000088554356,0.000050708077,0.000022670833,0.000031716965,0.000018098619],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001757796,0.00034004677,0.0002944553,0.00033280792,0.00024208923,0.0003515279,0.0007734,0.00064652145,0.0004338525],"category_scores_gemma":[0.00057700864,0.00023765408,0.00045707796,0.00027962626,0.0004503763,0.00071227015,0.00033484475,0.00030216973,0.000086766486],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003128934,0.000030619864,0.0019703323,0.000027902925,0.000013102417,0.000107542175,0.00005022598,0.9593513,0.03391146,0.0018522519,0.000035951383,0.0026180332],"study_design_scores_gemma":[0.0000023485534,0.000007861033,0.00031878854,0.0000012742515,0.0000020804096,0.000006528988,0.0000042902357,0.99814117,0.0013484892,0.0001251542,0.00003975942,0.0000021836338],"about_ca_topic_score_codex":0.0053803227,"about_ca_topic_score_gemma":0.0020005743,"teacher_disagreement_score":0.0053803227,"about_ca_system_score_codex":0.00047001973,"about_ca_system_score_gemma":0.0004586645,"threshold_uncertainty_score":0.01069802},"labels":[],"label_agreement":null},{"id":"W2738838206","doi":"10.1002/2017jb014045","title":"Combining periodic hydraulic tests and surface tilt measurements to explore in situ fracture hydromechanics","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Groundwater flow and contamination studies","field":"Environmental Science","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph","funders":"Agence Nationale de la Recherche; Equipex","keywords":"Geology; Bedrock; Tiltmeter; Geotechnical engineering; Stiffness; Tilt (camera); Mechanics; Hydraulic fracturing; Deformation (meteorology); Fracture (geology); Amplitude; Structural engineering; Engineering","score_opus":0.10404528126575385,"score_gpt":0.362695375335231,"score_spread":0.25865009406947714,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2738838206","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97256607,0.00016561773,0.025656492,0.000042907217,0.000037068283,0.00003256591,0.0004545256,0.00029616005,0.0007485264],"genre_scores_gemma":[0.9925955,0.00006431073,0.0069867815,0.00002508633,0.000010648084,0.000022503738,0.00011395985,0.000019715006,0.00016154136],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99978644,0.000018402803,0.000013879644,0.00005307324,0.00008274919,0.000045574747],"domain_scores_gemma":[0.9995988,0.00010896706,0.00008122394,0.00005606138,0.00011532948,0.000039516322],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032498784,0.0004749317,0.0003154751,0.00063155935,0.0001774021,0.00032264285,0.00032574998,0.00042640782,0.0013802989],"category_scores_gemma":[0.0005708432,0.00020994875,0.0002015813,0.00048851396,0.00038800063,0.0003932208,0.00046118035,0.0004274122,0.0002359884],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012240915,0.000076370314,0.02210349,0.00009256597,0.000025077654,0.00010763297,0.000095521544,0.0037265671,0.950775,0.00009059362,0.0001615009,0.022623323],"study_design_scores_gemma":[0.000025608131,0.0008659571,0.21152179,0.00003125908,0.000081723905,0.0002745315,0.0003867926,0.097928576,0.6867447,0.0005299263,0.0015100054,0.00009910723],"about_ca_topic_score_codex":0.00085139606,"about_ca_topic_score_gemma":0.002257639,"teacher_disagreement_score":0.0013802989,"about_ca_system_score_codex":0.00016780228,"about_ca_system_score_gemma":0.00018238052,"threshold_uncertainty_score":0.004617572},"labels":[],"label_agreement":null},{"id":"W2745230667","doi":"10.1002/2017jb014191","title":"Velocity models and hypocenter relocations for the Charlevoix Seismic Zone","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Hypocenter; Seismology; Rift; Impact structure; Devonian; Fault (geology); Basement; Shore; Tectonics; Paleontology; Induced seismicity","score_opus":0.1038744162207912,"score_gpt":0.3527415045320664,"score_spread":0.2488670883112752,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2745230667","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9768357,0.00007951491,0.018684609,0.000061332365,0.000008400935,0.00003865186,0.00087713916,0.0004410888,0.0029735556],"genre_scores_gemma":[0.99463236,0.000044808374,0.0033364145,0.0000035258365,0.0000022177553,0.000019703532,0.0010866987,0.000030012283,0.00084423844],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999007,0.000015138885,0.000005655974,0.000031959287,0.000026898306,0.000019598798],"domain_scores_gemma":[0.99976665,0.000040035437,0.00007535299,0.00002369342,0.00006240254,0.000031907377],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002843883,0.00049376616,0.00016957561,0.001065901,0.00037733707,0.0010190124,0.00077023514,0.00034997388,0.0012347949],"category_scores_gemma":[0.0007394453,0.00023487165,0.00029631087,0.000769021,0.00022935926,0.00026744916,0.00038491996,0.0003046946,0.00032840387],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014835024,0.00005070086,0.108303204,0.000015744441,0.000018912078,0.00014221226,0.00024548417,0.86734045,0.0026764786,0.0016067319,0.0008166925,0.018634979],"study_design_scores_gemma":[0.000020286403,0.000020172158,0.024839617,0.0000063829502,0.0000043225377,0.000028062037,0.0000835436,0.97309315,0.0008122657,0.0002913726,0.00078731996,0.000013472752],"about_ca_topic_score_codex":0.13658406,"about_ca_topic_score_gemma":0.07628493,"teacher_disagreement_score":0.86341596,"about_ca_system_score_codex":0.0021210194,"about_ca_system_score_gemma":0.0010743984,"threshold_uncertainty_score":0.27157807},"labels":[],"label_agreement":null},{"id":"W2752459840","doi":"10.1029/2017jb015394","title":"Direct Observation of Faulting by Means of Rotary Shear Tests Under X‐Ray Micro‐Computed Tomography","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; Canada Foundation for Innovation; Carbon Management Canada; CMG Reservoir Simulation Foundation","keywords":"Slip (aerodynamics); Shear (geology); Surface finish; Surface roughness; Interlocking; Tomography; Contact area; Power law","score_opus":0.05064586725670303,"score_gpt":0.3174288948849649,"score_spread":0.2667830276282619,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2752459840","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99727064,0.0000558792,0.0022604202,0.0000061251635,0.000002766246,0.000012891658,0.00009818279,0.000022317483,0.0002707023],"genre_scores_gemma":[0.9990073,0.000023569204,0.00083359075,0.0000028567968,0.000001449336,0.0000077683635,0.000030965155,0.0000023464077,0.00009019443],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9997861,0.000028800421,0.000018701548,0.0000514312,0.000077836004,0.000037146743],"domain_scores_gemma":[0.9991929,0.0002765661,0.00021707425,0.00013059388,0.000122021054,0.00006101015],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019529986,0.0002650622,0.00018427237,0.0004182062,0.00015621963,0.00024455576,0.00023081638,0.00020150404,0.0014879254],"category_scores_gemma":[0.00059520814,0.00014824898,0.00013703204,0.00025313947,0.0005663799,0.00018463575,0.00027281474,0.00022667545,0.000102076614],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012438846,0.00002792612,0.0063827774,0.000026296584,0.000006751834,0.000075992706,0.00005796545,0.00048736317,0.99061686,0.00004444734,0.000019516856,0.00212975],"study_design_scores_gemma":[0.000021933287,0.00090494496,0.1282519,0.0000072539265,0.00002368236,0.00027684117,0.00015062881,0.010077805,0.859945,0.000050863335,0.00027359056,0.000015519989],"about_ca_topic_score_codex":0.0010333428,"about_ca_topic_score_gemma":0.0012884352,"teacher_disagreement_score":0.0014879254,"about_ca_system_score_codex":0.0001318393,"about_ca_system_score_gemma":0.00010066292,"threshold_uncertainty_score":0.004977584},"labels":[],"label_agreement":null},{"id":"W2763119356","doi":"10.1002/2017jb014309","title":"TanDEM‐X Time Series Analysis Reveals Lava Flow Volume and Effusion Rates of the 2012–2013 Tolbachik, Kamchatka Fissure Eruption","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Synthetic Aperture Radar (SAR) Applications and Techniques","field":"Engineering","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Lava; Geology; Effusive eruption; Digital elevation model; Lava dome; Volcanology; Volcano; Lateral eruption; Volume (thermodynamics); Geomorphology; Remote sensing; Seismology; Magma; Explosive eruption","score_opus":0.016985086122947246,"score_gpt":0.31320865476927984,"score_spread":0.2962235686463326,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2763119356","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985397,0.000015692513,0.00022506533,0.000013578498,0.0000018790425,0.0000039015813,0.0008609205,0.000039617087,0.00029974032],"genre_scores_gemma":[0.9979297,0.0000118303515,0.00034579358,0.0000023791213,0.000002572885,0.000004997405,0.0015264753,0.00000412922,0.0001721169],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999403,0.0000049480063,0.0000046812797,0.000020946214,0.000017514525,0.000011694369],"domain_scores_gemma":[0.9998229,0.000024633991,0.00004832743,0.000019762469,0.00005888415,0.000025562393],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016960244,0.0001796804,0.00018747056,0.00086647295,0.00019104565,0.00029030832,0.0001748585,0.00027542483,0.00070719665],"category_scores_gemma":[0.0004226944,0.000097771976,0.00022878704,0.00093223044,0.00017824362,0.0002855299,0.00022678677,0.0001884311,0.00018302108],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00080342474,0.00029776755,0.8367509,0.00009878665,0.00019449824,0.0011736515,0.00090223027,0.04818507,0.052498937,0.0005359867,0.0039880467,0.054570585],"study_design_scores_gemma":[0.000009140827,0.000027561766,0.96859264,0.0000038960115,0.000018078947,0.000066434724,0.00014857126,0.028496753,0.002117949,0.000042982465,0.00046510398,0.0000109325865],"about_ca_topic_score_codex":0.016589163,"about_ca_topic_score_gemma":0.017520135,"teacher_disagreement_score":0.016589163,"about_ca_system_score_codex":0.00038183283,"about_ca_system_score_gemma":0.00017740091,"threshold_uncertainty_score":0.03298521},"labels":[],"label_agreement":null},{"id":"W2763912211","doi":"10.1002/2017jb014160","title":"Acoustic Reflectivity From Variously Oriented Orthorhombic Media: Analogies to Seismic Responses From a Fractured Anisotropic Crust","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; University of Alberta","keywords":"Azimuth; Anisotropy; Tilt (camera); Geology; Reflection (computer programming); Angle of incidence (optics); Optics; Reflectivity; Plane (geometry); Orientation (vector space); Geometry; Seismology; Physics; Mathematics; Computer science","score_opus":0.05449601199509864,"score_gpt":0.3570830565410581,"score_spread":0.30258704454595947,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2763912211","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99203193,0.0001158791,0.006039605,0.000023542783,0.000008983615,0.000016109858,0.000107955995,0.00008317233,0.0015728844],"genre_scores_gemma":[0.9986644,0.0000674344,0.0010955082,0.0000055308196,0.0000031427853,0.0000033845095,0.000044183453,0.000006846201,0.0001096795],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99982834,0.000029900224,0.000011394306,0.000028368797,0.00007421311,0.000027631728],"domain_scores_gemma":[0.99946433,0.00023986876,0.00011580914,0.00007745004,0.00006989838,0.00003255239],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041526154,0.00038966368,0.0002088841,0.00093606213,0.00011078852,0.00044537784,0.0003017877,0.00022897011,0.000836643],"category_scores_gemma":[0.0011722813,0.00023500762,0.0001508928,0.00063199346,0.0006016387,0.00024966014,0.00020262264,0.0002992398,0.00017232294],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028288734,0.000071534254,0.0054869293,0.00009442685,0.00002914709,0.00040396472,0.00019660659,0.008599204,0.97532314,0.001042773,0.000077061006,0.008392276],"study_design_scores_gemma":[0.000091946225,0.00063899334,0.11540964,0.000031448784,0.00010064436,0.0012432294,0.00073213386,0.14718828,0.7314051,0.0017574112,0.001306754,0.0000943509],"about_ca_topic_score_codex":0.0007196149,"about_ca_topic_score_gemma":0.0008596248,"teacher_disagreement_score":0.00093606213,"about_ca_system_score_codex":0.00015287398,"about_ca_system_score_gemma":0.000087406435,"threshold_uncertainty_score":0.0027988553},"labels":[],"label_agreement":null},{"id":"W2765095838","doi":"10.1002/2017jb014578","title":"Seismologically Observed Spatiotemporal Drainage Activity at Moulins","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Simon Fraser University; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; University of Minnesota; Japan Society for the Promotion of Science; Simon Fraser University; Canada Research Chairs; California Institute of Technology; Parks Canada; National Science Foundation","keywords":"Geology; Geophone; Meltwater; Glacier; Ambient noise level; Passive seismic; Seismology; Noise (video); Seismic noise; Microearthquake; Geomorphology; Induced seismicity; Sound (geography)","score_opus":0.13943848135724418,"score_gpt":0.3621996780769833,"score_spread":0.2227611967197391,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2765095838","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99932456,0.000012171534,0.00019562556,0.0000041003877,6.837734e-7,0.0000025301297,0.00016480772,0.00001293786,0.00028262864],"genre_scores_gemma":[0.99937385,0.000016157815,0.00016870358,0.0000019291613,0.0000011502708,0.000003289162,0.00031307378,0.0000033869915,0.000118427444],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999136,0.000007710092,0.0000045700303,0.000028152632,0.000017770652,0.000028220747],"domain_scores_gemma":[0.9998023,0.000026384809,0.00005284468,0.000016502392,0.000060158876,0.000041854004],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012684512,0.0002540326,0.00022744833,0.0014512851,0.00034982726,0.00049872097,0.00025460534,0.00025555943,0.00058109633],"category_scores_gemma":[0.00051583425,0.000118666496,0.000116690346,0.0011444984,0.00029320366,0.00019543545,0.00053196884,0.00013282821,0.000109908426],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002089404,0.000056462595,0.91992426,0.000028627495,0.000097352284,0.0003182118,0.00072928617,0.007906537,0.053106286,0.0001998326,0.00029233008,0.017131822],"study_design_scores_gemma":[0.0000031697934,0.000016616754,0.9948826,0.000004455969,0.000010616349,0.000026932634,0.00019416682,0.0035166298,0.0010826032,0.000017975854,0.00023947768,0.00000495474],"about_ca_topic_score_codex":0.031988375,"about_ca_topic_score_gemma":0.07149762,"teacher_disagreement_score":0.031988375,"about_ca_system_score_codex":0.00043148402,"about_ca_system_score_gemma":0.00035425683,"threshold_uncertainty_score":0.063604355},"labels":[],"label_agreement":null},{"id":"W2765169709","doi":"10.1002/2017jb014618","title":"Earthquakes in the Mantle? Insights From Rock Magnetism of Pseudotachylytes","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"Norges Forskningsråd; National Sleep Foundation","keywords":"Ultramafic rock; Geology; Magnetite; Mantle (geology); Geochemistry; Magnetism; Peridotite; Condensed matter physics; Paleontology; Physics","score_opus":0.030655782184271306,"score_gpt":0.33235108928720175,"score_spread":0.30169530710293047,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2765169709","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990711,0.00016494341,0.00013957534,0.000021822036,0.000001249538,8.969862e-7,0.000042472337,0.00000629928,0.0005515242],"genre_scores_gemma":[0.9997172,0.000062406296,0.00009597108,0.0000057426023,0.0000019703803,5.344596e-7,0.00003382355,0.0000018177736,0.000080497615],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99997795,0.000002806693,0.0000020586556,0.0000067026926,0.0000055796886,0.0000048680927],"domain_scores_gemma":[0.99993765,0.000011090292,0.000026662721,0.000006340584,0.000009219999,0.000009041762],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006135395,0.00011568811,0.0001239141,0.0005370332,0.00014331439,0.0003888862,0.00014114691,0.0002120994,0.0010399098],"category_scores_gemma":[0.00020573751,0.000114198374,0.00007640826,0.00037908106,0.00029159794,0.00029283212,0.00027631514,0.00013134204,0.00011491726],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040049374,0.000024645564,0.20029211,0.00013577547,0.00003410107,0.0005560369,0.0012451536,0.00054482993,0.77856666,0.0012667603,0.0000850034,0.016848521],"study_design_scores_gemma":[0.0000097591155,0.00007832294,0.9850647,0.0000075381827,0.000014640923,0.00046673795,0.0005545143,0.0010230227,0.0111166695,0.0005227371,0.0011350649,0.000006350681],"about_ca_topic_score_codex":0.0013437746,"about_ca_topic_score_gemma":0.0029092266,"teacher_disagreement_score":0.0013437746,"about_ca_system_score_codex":0.00016485766,"about_ca_system_score_gemma":0.00007360186,"threshold_uncertainty_score":0.0034788847},"labels":[],"label_agreement":null},{"id":"W2765726846","doi":"10.1002/2017jb014808","title":"Lakes as a Source of Short‐Period (0.5–2 s) Microseisms","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Natural Science Foundation of China","keywords":"Microseism; Shore; Geology; Wind wave; Seismology; Climatology; Oceanography","score_opus":0.04388740690189393,"score_gpt":0.34482867201049316,"score_spread":0.30094126510859925,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2765726846","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99886143,0.00004324572,0.00023726899,0.000013966954,0.0000015391329,0.0000032821968,0.00013728725,0.000013645374,0.00068821],"genre_scores_gemma":[0.9993662,0.000017482565,0.00024277034,0.0000038721514,0.0000020850734,0.000003574552,0.000121003235,0.0000030732654,0.00023994427],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994075,0.000004189077,0.0000038138705,0.000009981327,0.000023320228,0.000017878536],"domain_scores_gemma":[0.9997991,0.000024576573,0.00008787622,0.000010273668,0.000050819002,0.000027479187],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009001167,0.00012455309,0.000078809615,0.0008059642,0.00039494477,0.00036297846,0.00014322122,0.00013735543,0.0008205934],"category_scores_gemma":[0.00031570886,0.00010529977,0.00010227937,0.00095532904,0.00032018285,0.00023165594,0.00046832763,0.00009322688,0.00007558169],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014671178,0.000017763361,0.94283736,0.000052682684,0.00006778332,0.0005231505,0.0015523596,0.0014842986,0.039235085,0.00040288456,0.00069528114,0.012984571],"study_design_scores_gemma":[0.0000028937507,0.00001025409,0.9961824,0.0000031620975,0.000011366926,0.000047257337,0.00021839344,0.0014432289,0.001308168,0.000054159056,0.0007141841,0.0000045217917],"about_ca_topic_score_codex":0.021908589,"about_ca_topic_score_gemma":0.06490338,"teacher_disagreement_score":0.021908589,"about_ca_system_score_codex":0.0004286068,"about_ca_system_score_gemma":0.0004085483,"threshold_uncertainty_score":0.043562114},"labels":[],"label_agreement":null},{"id":"W2766232693","doi":"10.1002/2017jb014074","title":"Hydromechanical Modeling of Stress, Pore Pressure, and Porosity Evolution in Fold‐and‐Thrust Belt Systems","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"Total; Universiti Teknologi Petronas; Statoil; European Network and Information Security Agency; Petrobras; BG Group; ConocoPhillips; DONG Energy; Chevron; BP","keywords":"Anticline; Geology; Overpressure; Pore water pressure; Porosity; Thrust; Stress field; Fold and thrust belt; Overburden pressure; Thrust fault; Fold (higher-order function); Hydrostatic equilibrium; Compaction; Geotechnical engineering; Petrology; Stress (linguistics); Tectonics; Finite element method; Seismology; Structural engineering","score_opus":0.053527211597544665,"score_gpt":0.3202014406087605,"score_spread":0.26667422901121585,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2766232693","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99605477,0.000021602042,0.0022774565,0.00007594527,0.000004889697,0.000011045814,0.00010406804,0.000043047366,0.0014071894],"genre_scores_gemma":[0.9990501,0.000012426897,0.00061942684,0.0000110916535,0.0000025140216,0.0000135727205,0.000047114336,0.000009847676,0.00023393315],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992955,0.000015226242,0.000003483658,0.000013361577,0.000012486495,0.000025873973],"domain_scores_gemma":[0.9997079,0.00013873188,0.00004288231,0.000020096235,0.000037297326,0.00005311798],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021565538,0.00039514873,0.00042009357,0.0005014416,0.0005805331,0.00079334644,0.00092017907,0.0011170364,0.0012665928],"category_scores_gemma":[0.0009707041,0.00032371073,0.00053856586,0.00029740107,0.0011931065,0.0005832312,0.00051179325,0.00045371306,0.00008291358],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000030741045,0.00004231524,0.0033942387,0.000008452933,0.000016872791,0.000064405125,0.000038209022,0.99329996,0.0019283699,0.000697677,0.000043357897,0.00043545992],"study_design_scores_gemma":[0.000016136342,0.000012614834,0.0011325154,0.0000011704321,0.0000032801734,0.0000045444117,0.000012810361,0.9983808,0.00024071403,0.0001523801,0.000039503044,0.000003417626],"about_ca_topic_score_codex":0.03569665,"about_ca_topic_score_gemma":0.012075871,"teacher_disagreement_score":0.03569665,"about_ca_system_score_codex":0.0017737488,"about_ca_system_score_gemma":0.0010036606,"threshold_uncertainty_score":0.07097775},"labels":[],"label_agreement":null},{"id":"W2766698211","doi":"10.1002/2017jb014303","title":"Mobility Effect on Poroelastic Seismic Signatures in Partially Saturated Rocks With Applications in Time‐Lapse Monitoring of a Heavy Oil Reservoir","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"National Natural Science Foundation of China; Cenovus Energy","keywords":"Poromechanics; Geology; Saturation (graph theory); Compressibility; Pore water pressure; Mesoscopic physics; Geophysical imaging; Fluid dynamics; Petrology; Porous medium; Porosity; Mineralogy; Mechanics; Geophysics; Geotechnical engineering","score_opus":0.02234066114981383,"score_gpt":0.3146338796159109,"score_spread":0.29229321846609707,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2766698211","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99446374,0.0000552437,0.005009491,0.000020163925,0.0000025285428,0.000004561667,0.000108229615,0.00005760274,0.00027850948],"genre_scores_gemma":[0.9963296,0.000051899162,0.0033965323,0.000003547056,0.0000028998363,0.0000039609763,0.000084990876,0.000007165134,0.00011941469],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999399,0.0000068949003,0.0000037551831,0.000020133093,0.000017537166,0.000011766701],"domain_scores_gemma":[0.9998398,0.00004823983,0.000043767235,0.00001612847,0.000030238429,0.000021811145],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016144678,0.00030469112,0.00021912968,0.0006839425,0.00014661544,0.00020253746,0.00029086188,0.00027567858,0.00053024845],"category_scores_gemma":[0.0003856288,0.00013370211,0.00016305901,0.0005983918,0.0002228632,0.00026693635,0.0002833458,0.00018296279,0.00007238013],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005797733,0.00014237253,0.049392283,0.00024460925,0.00007676797,0.0010438184,0.00048175856,0.04447675,0.8665708,0.00035587855,0.0002120143,0.03642316],"study_design_scores_gemma":[0.000028541288,0.00040270924,0.19845214,0.000036545443,0.00012479466,0.00075696234,0.0005421149,0.52253526,0.2756965,0.0003612679,0.0009874732,0.00007567512],"about_ca_topic_score_codex":0.0020955945,"about_ca_topic_score_gemma":0.0029100566,"teacher_disagreement_score":0.0020955945,"about_ca_system_score_codex":0.000117354735,"about_ca_system_score_gemma":0.00012202999,"threshold_uncertainty_score":0.004166782},"labels":[],"label_agreement":null},{"id":"W2767779763","doi":"10.1002/2017jb014946","title":"Seismicity During the Initial Stages of the Guy‐Greenbrier, Arkansas, Earthquake Sequence","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":74,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Lawrence Livermore National Laboratory; Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ; U.S. Geological Survey; National Science Foundation; University of Cambridge; British Columbia Oil and Gas Commission; National Science Foundation of Sri Lanka","keywords":"Induced seismicity; Seismology; Geology; Hydraulic fracturing; Seismic hazard; Waveform; Fault (geology); Geotechnical engineering; Engineering","score_opus":0.08908635233086566,"score_gpt":0.361341438118219,"score_spread":0.27225508578735336,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2767779763","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99846965,0.00003111662,0.00010353192,0.000020150015,0.0000013267759,0.0000042681736,0.00090143527,0.000050168,0.00041832734],"genre_scores_gemma":[0.9982003,0.000018574417,0.00013700209,0.000006160859,0.000003189832,0.000006348102,0.0014278219,0.0000035173955,0.00019705284],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998907,0.000012425983,0.0000092042,0.000028205062,0.000024387085,0.000035063855],"domain_scores_gemma":[0.9995925,0.0000522617,0.00015944005,0.000023514582,0.000081028156,0.00009126928],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012455974,0.00013483452,0.0001551002,0.00095698016,0.00033682803,0.00036604496,0.00020428981,0.00026149355,0.0008849048],"category_scores_gemma":[0.0004119121,0.00008407105,0.0001143603,0.0007947122,0.00021214108,0.00017733767,0.0003633723,0.00019049777,0.00020751514],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00059267937,0.00010772783,0.959955,0.00005422974,0.00005490358,0.00070208387,0.0006544497,0.00512482,0.018835125,0.000068812,0.0016571718,0.01219309],"study_design_scores_gemma":[0.0000039743522,0.000030417092,0.99811375,0.0000022487643,0.0000062625295,0.0000294672,0.00015981922,0.0010308082,0.00037061455,0.000005136307,0.00024346964,0.000004024972],"about_ca_topic_score_codex":0.050053142,"about_ca_topic_score_gemma":0.12688056,"teacher_disagreement_score":0.050053142,"about_ca_system_score_codex":0.00052773085,"about_ca_system_score_gemma":0.00038001296,"threshold_uncertainty_score":0.099523604},"labels":[],"label_agreement":null},{"id":"W2767881733","doi":"10.1002/2017jb014474","title":"Magnetotelluric Imaging of Lower Crustal Melt and Lithospheric Hydration in the Rocky Mountain Front Transition Zone, Colorado, USA","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"National Science Foundation of Sri Lanka; University of Colorado Boulder; U.S. Forest Service; Geological Society of America; U.S. Geological Survey; National Science Foundation; Australian Society of Exploration Geophysicists Research Foundation; University of Alberta","keywords":"Geology; Lithosphere; Magnetotellurics; Crust; Mantle (geology); Rift; Tectonics; North American Plate; Geochemistry; Plate tectonics; Paleontology; Electrical resistivity and conductivity","score_opus":0.02723837663806447,"score_gpt":0.321489420450712,"score_spread":0.29425104381264755,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2767881733","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997652,0.00006224852,0.00053433,0.00006350666,0.0000013312219,0.0000054138623,0.00052713073,0.000044056822,0.0011100528],"genre_scores_gemma":[0.9983955,0.000038697683,0.0007003835,0.00001545912,0.0000026288888,0.000006199434,0.0005516416,0.0000057631537,0.00028362437],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999585,0.000004814479,0.0000011326484,0.000014208688,0.000009253117,0.000011993224],"domain_scores_gemma":[0.9999242,0.0000066068974,0.000013478172,0.000005990836,0.00003642315,0.0000132157165],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008953972,0.00012736277,0.000115516144,0.00045355523,0.00042246177,0.00032879453,0.0002502791,0.00028398325,0.0005507801],"category_scores_gemma":[0.00015169475,0.000120276774,0.000093668954,0.00038018214,0.00015222204,0.00015177738,0.00019919603,0.000161625,0.00011102944],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023772552,0.00011653989,0.8014356,0.000068771005,0.00013687668,0.00037915393,0.0009347751,0.012743592,0.16299279,0.00026789957,0.002281644,0.018404655],"study_design_scores_gemma":[0.000014468971,0.000021266733,0.97989833,0.000009305414,0.000016968015,0.00008132074,0.0003336814,0.016021933,0.0026197212,0.000045711044,0.000928233,0.000008970821],"about_ca_topic_score_codex":0.13974126,"about_ca_topic_score_gemma":0.2871642,"teacher_disagreement_score":0.13974126,"about_ca_system_score_codex":0.0004953284,"about_ca_system_score_gemma":0.00040344655,"threshold_uncertainty_score":0.2778557},"labels":[],"label_agreement":null},{"id":"W2768809495","doi":"10.1002/2017jb014710","title":"The Role of Texture, Cracks, and Fractures in Highly Anisotropic Shales","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Nexen (Canada)","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Anisotropy; Geology; Isotropy; Seismic anisotropy; Hydraulic fracturing; Shear wave splitting; Transverse isotropy; Oil shale; Fracture (geology); Lithology; Shear (geology); Texture (cosmology); Microseism; Mineralogy; Geophysics; Seismology; Geotechnical engineering; Petrology; Optics; Physics; Mantle (geology)","score_opus":0.02196153035140153,"score_gpt":0.32672588072374936,"score_spread":0.30476435037234784,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2768809495","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99963987,0.0000122126685,0.00020594479,0.000004110719,2.102743e-7,8.575531e-7,0.000015933594,0.0000055522532,0.00011520187],"genre_scores_gemma":[0.99982846,0.000005152506,0.00010863606,9.099546e-7,4.8370345e-7,5.571509e-7,0.000012632102,0.0000013675105,0.000041857933],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998652,0.000015778469,0.000009587254,0.000036256733,0.00003792928,0.000035277153],"domain_scores_gemma":[0.99945873,0.00012458074,0.00019117004,0.000039703657,0.00011422341,0.00007155155],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018790453,0.00016679124,0.00016141123,0.000988636,0.0003372761,0.0004484532,0.00016569655,0.0002939479,0.0006001244],"category_scores_gemma":[0.0004760698,0.0003194529,0.000096114694,0.00032144267,0.00058595755,0.00025036954,0.00029112375,0.00012985352,0.000079271806],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024890658,0.00005161836,0.447461,0.000049982256,0.00003732682,0.000422328,0.0003934436,0.004402753,0.5394063,0.00038626336,0.000056549823,0.0070835417],"study_design_scores_gemma":[0.0000076280253,0.000058618025,0.9679294,0.000004563372,0.0000125783,0.00025348226,0.00023832379,0.014848327,0.01629791,0.00017370017,0.00016305955,0.000012344462],"about_ca_topic_score_codex":0.0044331127,"about_ca_topic_score_gemma":0.0073161507,"teacher_disagreement_score":0.0044331127,"about_ca_system_score_codex":0.00026522396,"about_ca_system_score_gemma":0.00017039785,"threshold_uncertainty_score":0.008814633},"labels":[],"label_agreement":null},{"id":"W2768939228","doi":"10.1002/2016jb013844","title":"Comment on “An Assessment of the ICE‐6G_C (VM5a) Glacial Isostatic Adjustment Model” by Purcell et al.","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":511,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; University of Toronto","keywords":"Geology; Post-glacial rebound; Spherical harmonics; Radiocarbon dating; Geodesy; Glacial period; Bathymetry; Ice sheet; Last Glacial Maximum; Paleontology; Oceanography; Physics","score_opus":0.08180941149715669,"score_gpt":0.39981165542520686,"score_spread":0.31800224392805015,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2768939228","genre_codex":"commentary","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":"commentary","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0011784278,0.0017011442,0.0014129838,0.88628316,0.10356134,0.00004068805,0.0013419068,0.0004263134,0.0040540574],"genre_scores_gemma":[0.012836525,0.0013671247,0.0016294337,0.91560745,0.059601214,0.00012889937,0.00053497835,0.0004590538,0.007835284],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9952016,0.0009432766,0.000722105,0.0009127592,0.0018071341,0.0004131182],"domain_scores_gemma":[0.97574514,0.009356336,0.0016905834,0.0012701579,0.010739409,0.0011984032],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0068759127,0.0014066771,0.0010011904,0.001147788,0.0030804467,0.0030904836,0.005832753,0.018296527,0.013055393],"category_scores_gemma":[0.060242873,0.00075348094,0.001420261,0.0015864628,0.00329894,0.0049289004,0.0023364816,0.02101175,0.01090887],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000028022154,0.0000074616178,0.00032850145,0.000050653132,0.000009793521,0.00011440111,0.00012907633,0.00012511187,0.00009047119,0.0013496223,0.9951663,0.0026006203],"study_design_scores_gemma":[0.000050145998,0.000030891108,0.0020587316,0.0003667345,0.00003225625,0.00030224034,0.0005860909,0.00080121355,0.0011347845,0.004903008,0.98961735,0.000116556475],"about_ca_topic_score_codex":0.04974345,"about_ca_topic_score_gemma":0.023469804,"teacher_disagreement_score":0.04974345,"about_ca_system_score_codex":0.0031738305,"about_ca_system_score_gemma":0.004200456,"threshold_uncertainty_score":0.09890783},"labels":[],"label_agreement":null},{"id":"W2770339755","doi":"10.1002/2017jb014695","title":"The Influence of Sediment Isostatic Adjustment on Sea Level Change and Land Motion Along the U.S. Gulf Coast","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland; University of Ottawa","funders":"University of Ottawa","keywords":"Post-glacial rebound; Tide gauge; Geology; Subsidence; Sea level; Tectonic uplift; Latitude; Sediment; Geodesy; Physical geography; Climatology; Oceanography; Geomorphology; Tectonics; Seismology; Geography","score_opus":0.12993348241731545,"score_gpt":0.3381400447647428,"score_spread":0.20820656234742735,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2770339755","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992205,0.000021087637,0.00017416642,0.000043363412,0.0000022801053,0.0000014608366,0.00013242783,0.000011562161,0.0003932306],"genre_scores_gemma":[0.9996613,0.000017022177,0.00009403351,0.0000074430723,0.000001026498,0.0000013232791,0.00012744823,0.000003587299,0.00008665772],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989283,0.00003533972,0.000008743967,0.000029094623,0.000016731983,0.000017335771],"domain_scores_gemma":[0.9995425,0.00017591666,0.00009089642,0.000047108708,0.00007424596,0.000069342],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037368535,0.00030956397,0.0001667887,0.00041714814,0.00030372388,0.0007758016,0.00033494466,0.00035398183,0.00075279665],"category_scores_gemma":[0.0015356708,0.00028645617,0.00035606403,0.00035674425,0.00033524592,0.00030806012,0.00038616758,0.00025478672,0.00010980031],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014847134,0.000072339484,0.6179777,0.000017010729,0.000116409086,0.00012070185,0.00007251106,0.37330735,0.0016186937,0.0005589683,0.00043232462,0.005557673],"study_design_scores_gemma":[0.000027683785,0.000078848716,0.35373494,0.000014504649,0.0000432395,0.000036071768,0.00008972139,0.64451385,0.0007210228,0.00029794226,0.0004223248,0.000019812065],"about_ca_topic_score_codex":0.108256444,"about_ca_topic_score_gemma":0.07606193,"teacher_disagreement_score":0.108256444,"about_ca_system_score_codex":0.0012485933,"about_ca_system_score_gemma":0.00061449915,"threshold_uncertainty_score":0.2152527},"labels":[],"label_agreement":null},{"id":"W2771620931","doi":"10.1002/2017jb015019","title":"Linear Array Ambient Noise Adjoint Tomography Reveals Intense Crust‐Mantle Interactions in North China Craton","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; China Earthquake Administration; China Scholarship Council; Compute Canada; Canada Foundation for Innovation; National Natural Science Foundation of China; University of Toronto; Government of Ontario","keywords":"Geology; Seismic tomography; Crust; Tomography; Mantle (geology); Ambient noise level; Craton; Geophysics; Seismology; Physics; Tectonics; Optics; Geomorphology","score_opus":0.04683859988419193,"score_gpt":0.3437666593505475,"score_spread":0.2969280594663556,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2771620931","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9854107,0.000036412617,0.013062202,0.000060123755,0.0000059849244,0.000007709452,0.00018208759,0.00017105757,0.0010637142],"genre_scores_gemma":[0.9942485,0.000015847689,0.005219285,0.000014407238,0.0000046541054,0.000005778913,0.00012212122,0.000013840039,0.00035558152],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99994147,0.0000057813822,0.0000027216834,0.000018699837,0.000018221297,0.000013049598],"domain_scores_gemma":[0.99993026,0.000008786859,0.000014939385,0.000008603784,0.000026578417,0.00001088358],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011210842,0.00027707938,0.00014063477,0.0005171756,0.00016007929,0.00030508704,0.00023593103,0.000265378,0.0009908694],"category_scores_gemma":[0.00027755898,0.00019816398,0.00018072748,0.0003890071,0.00025081393,0.00025156882,0.0004072141,0.00017406701,0.00012284491],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00049554283,0.00012127863,0.29685733,0.00013126334,0.00014436903,0.0017713837,0.0012325613,0.13646369,0.47801396,0.001996994,0.0011079148,0.0816636],"study_design_scores_gemma":[0.000043560685,0.00009299133,0.4978095,0.000024472223,0.00010273579,0.00046787327,0.000620489,0.47519663,0.023036659,0.0009402205,0.0015839228,0.000080830956],"about_ca_topic_score_codex":0.010958012,"about_ca_topic_score_gemma":0.016222235,"teacher_disagreement_score":0.010958012,"about_ca_system_score_codex":0.0002068013,"about_ca_system_score_gemma":0.00044510642,"threshold_uncertainty_score":0.021788478},"labels":[],"label_agreement":null},{"id":"W2777940559","doi":"10.1002/2017jb014741","title":"Post‐rift Tectonic History of the Songliao Basin, NE China: Cooling Events and Post‐rift Unconformities Driven by Orogenic Pulses From Plate Boundaries","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"National Natural Science Foundation of China","keywords":"Unconformity; Geology; Rift; Paleontology; Cretaceous; Thermochronology; Fission track dating; Tectonics; Cenozoic; Thermal subsidence; Structural basin; Plate tectonics; Tectonic uplift","score_opus":0.018641872992687065,"score_gpt":0.2572590614494445,"score_spread":0.23861718845675742,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2777940559","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99949944,0.00007986399,0.000035115183,0.000010455635,7.884198e-7,0.0000015944253,0.000074280295,0.000002787107,0.00029563732],"genre_scores_gemma":[0.9997156,0.000042048046,0.000027007547,0.0000034109285,0.000001779546,0.000001541916,0.0000889535,9.950004e-7,0.00011863267],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993837,0.000005226376,0.000007370821,0.000021661672,0.000009766623,0.000017584718],"domain_scores_gemma":[0.9997869,0.000021777088,0.00008183432,0.000014366417,0.000052751322,0.000042223233],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020464306,0.00019358308,0.00015253617,0.0009497906,0.00046288123,0.000386441,0.0002051647,0.00014375604,0.00078086887],"category_scores_gemma":[0.00033114193,0.00011161328,0.00012277933,0.0010169176,0.00044591326,0.00025592005,0.00028609153,0.00011200776,0.00006398637],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000067245724,0.000012045575,0.9734561,0.000048102687,0.000051225365,0.00027452465,0.0009445448,0.00077176787,0.011891194,0.000302605,0.000099905476,0.012080866],"study_design_scores_gemma":[0.0000012643927,0.0000061516394,0.99920005,0.0000021471403,0.0000051286843,0.000024529216,0.00007397835,0.0003830982,0.00016194874,0.00001973502,0.00012048789,0.0000015277648],"about_ca_topic_score_codex":0.052701764,"about_ca_topic_score_gemma":0.09552583,"teacher_disagreement_score":0.052701764,"about_ca_system_score_codex":0.00083244784,"about_ca_system_score_gemma":0.0005608743,"threshold_uncertainty_score":0.10479003},"labels":[],"label_agreement":null},{"id":"W2779742602","doi":"10.1002/2017jb014911","title":"Segmentation of Slow Slip Events in South Central Alaska Possibly Controlled by a Subducted Oceanic Plateau","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Research Foundation of Korea; Natural Sciences and Engineering Research Council of Canada; Korea Meteorological Administration; National Science Foundation","keywords":"Geology; Subduction; Seismology; Slip (aerodynamics); Plateau (mathematics); Fault (geology); Slab; Tectonics; Geophysics","score_opus":0.03350542124215864,"score_gpt":0.31892817447306965,"score_spread":0.285422753230911,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2779742602","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99967396,0.000013252894,0.00006686487,0.000004880417,5.7472766e-7,0.0000015301637,0.000024019642,0.000004360607,0.00021045233],"genre_scores_gemma":[0.9998846,0.000008016016,0.00003605393,7.383894e-7,4.999004e-7,0.0000012018057,0.000034497065,8.230803e-7,0.000033616958],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999293,0.000012315788,0.000008349705,0.000024499923,0.0000090918375,0.000016416532],"domain_scores_gemma":[0.9997464,0.000055051496,0.00009670614,0.000018044657,0.000031541564,0.00005222899],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016743389,0.00015342803,0.00019450707,0.0006394077,0.000347012,0.0005395966,0.00020964148,0.00026256882,0.0008178393],"category_scores_gemma":[0.0007034102,0.0001458164,0.00024408127,0.00041223576,0.00042079418,0.00028892138,0.00037478792,0.00012022506,0.0000847441],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002764776,0.000052514966,0.9628118,0.000033983615,0.000082317994,0.00088520313,0.0006037554,0.019752571,0.011643374,0.0005574976,0.00009248149,0.003208052],"study_design_scores_gemma":[0.000011325094,0.00005740634,0.96814716,0.000010952305,0.000026630212,0.00009224767,0.00061023154,0.03009809,0.0005233888,0.00028653667,0.00012431265,0.000011732753],"about_ca_topic_score_codex":0.020941885,"about_ca_topic_score_gemma":0.021715991,"teacher_disagreement_score":0.020941885,"about_ca_system_score_codex":0.0005254341,"about_ca_system_score_gemma":0.00033377067,"threshold_uncertainty_score":0.041639984},"labels":[],"label_agreement":null},{"id":"W2783221544","doi":"10.1002/2017jb014846","title":"Inverse Problems in Geodynamics Using Machine Learning Algorithms","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Directorate for Computer and Information Science and Engineering; National Sleep Foundation; National Science Foundation","keywords":"Geodynamics; Geophysics; Algorithm; Machine learning; Mantle convection; Mantle (geology); Artificial intelligence; Geology; Computer science; Inverse; Mathematics; Geometry","score_opus":0.054135131629005795,"score_gpt":0.3293522305349888,"score_spread":0.275217098905983,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2783221544","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0056810435,0.0009132018,0.9908285,0.0005859026,0.000052187694,0.000027049611,0.00004138383,0.00019440794,0.0016763363],"genre_scores_gemma":[0.44678816,0.0013785223,0.5459124,0.0003430803,0.00043695874,0.00039737314,0.0002838184,0.000107833126,0.0043518445],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9991425,0.0004709799,0.000049003494,0.00012264465,0.00017164343,0.000043181884],"domain_scores_gemma":[0.99266243,0.0061585302,0.00036125703,0.00020371293,0.0005221381,0.00009200661],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002367208,0.0010011999,0.0013691174,0.0013759276,0.00053817383,0.0016481839,0.001087331,0.0019699475,0.0025388761],"category_scores_gemma":[0.00960986,0.00062068814,0.0009400442,0.0012644033,0.0017880021,0.0013717911,0.0017416584,0.0021647832,0.000511138],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017092061,0.000029225637,0.0005914163,0.00008628382,0.00003565677,0.000031026502,0.000030464023,0.946705,0.00022865282,0.02123044,0.00075372617,0.03026106],"study_design_scores_gemma":[0.0000025813374,0.0000031256357,0.00002442802,0.0000052629107,8.634968e-7,0.0000026419752,0.000001956133,0.99054915,0.000035921763,0.009219175,0.00015334462,0.0000016022631],"about_ca_topic_score_codex":0.0052570556,"about_ca_topic_score_gemma":0.003277198,"teacher_disagreement_score":0.0052570556,"about_ca_system_score_codex":0.0010147252,"about_ca_system_score_gemma":0.0012220575,"threshold_uncertainty_score":0.012519181},"labels":[],"label_agreement":null},{"id":"W2787028490","doi":"10.1002/2017jb015021","title":"Seismicity Relocation and Fault Structure Near the Leech River Fault Zone, Southern Vancouver Island","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; McGill University","funders":"Fonds de recherche du Québec – Nature et technologies","keywords":"Geology; Seismology; Induced seismicity; Fault (geology); Sinistral and dextral; Seismometer; Active fault; Fault trace; Crust; Paleontology","score_opus":0.022358002500154548,"score_gpt":0.2876856933844599,"score_spread":0.2653276908843053,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2787028490","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980761,0.00007435044,0.000072965864,0.000020822219,0.000001557432,0.000009760276,0.0006024615,0.000009016498,0.0011328696],"genre_scores_gemma":[0.99792176,0.00007629412,0.00021657783,0.000011870785,9.575981e-7,0.000007908892,0.0008550267,0.0000030776043,0.00090665906],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998325,0.000008604372,0.0000080906475,0.00005495264,0.00005129027,0.000044492197],"domain_scores_gemma":[0.9995352,0.00002579005,0.0000876485,0.000023895109,0.00021838016,0.000109068875],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012576084,0.00021091584,0.00015597254,0.0014403249,0.0009974237,0.00085027877,0.00032062578,0.00024749892,0.0012011051],"category_scores_gemma":[0.0004932487,0.00015288316,0.00009395164,0.0015940616,0.0004206546,0.00014186988,0.0005713563,0.00024232618,0.00018878467],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004356585,0.000014981947,0.97763467,0.00003639216,0.000036275043,0.00023257744,0.0011402242,0.0005506675,0.007188778,0.000061891165,0.00042155644,0.012638483],"study_design_scores_gemma":[0.0000013773309,0.0000039454253,0.9984156,0.0000068992567,0.0000036225217,0.0000316736,0.0007583204,0.0002003038,0.00015949628,0.0000062997105,0.00041000743,0.0000024894073],"about_ca_topic_score_codex":0.84553254,"about_ca_topic_score_gemma":0.96046543,"teacher_disagreement_score":0.15446746,"about_ca_system_score_codex":0.0028675813,"about_ca_system_score_gemma":0.002395795,"threshold_uncertainty_score":0.31075424},"labels":[],"label_agreement":null},{"id":"W2789354433","doi":"10.1002/2017jb015138","title":"Archie's Saturation Exponent for Natural Gas Hydrate in Coarse‐Grained Reservoirs","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":120,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Government of Canada; Natural Resources Canada; U.S. Geological Survey; U.S. Department of Energy","keywords":"Permafrost; Clathrate hydrate; Saturation (graph theory); Geology; Hydrate; Natural gas; Mineralogy; Geotechnical engineering; Chemistry; Oceanography; Mathematics","score_opus":0.03323583098798739,"score_gpt":0.3361581232514136,"score_spread":0.3029222922634262,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2789354433","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9669307,0.00038241348,0.021467395,0.00028715373,0.000024016295,0.00007075861,0.000889789,0.0006253749,0.009322437],"genre_scores_gemma":[0.998156,0.00004239028,0.0012003656,0.000024095641,0.0000026873645,0.000011689087,0.0001273006,0.000019451432,0.00041598952],"study_design_codex":"observational","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99974936,0.000017358992,0.000018129991,0.000071483,0.00008504235,0.000058528967],"domain_scores_gemma":[0.9980731,0.0007884188,0.0003319731,0.00018855068,0.00051956845,0.00009839646],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006863003,0.00027676308,0.00017992212,0.0020053268,0.00035976252,0.00049530197,0.00077250507,0.00036876852,0.0022542002],"category_scores_gemma":[0.0048900954,0.00025869807,0.0002982708,0.0006749189,0.0008063106,0.0013173937,0.0006597089,0.00047700168,0.0003765237],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006020604,0.00024440206,0.56537026,0.00035184418,0.00017331718,0.0010372957,0.0019276318,0.21234411,0.10874497,0.01758647,0.0060110064,0.08560657],"study_design_scores_gemma":[0.000036616668,0.00012842221,0.22041245,0.00006698217,0.000042084557,0.00026136317,0.00070016785,0.71742034,0.051207528,0.0056109424,0.0040128557,0.00010031757],"about_ca_topic_score_codex":0.04025791,"about_ca_topic_score_gemma":0.027053999,"teacher_disagreement_score":0.04025791,"about_ca_system_score_codex":0.0014516963,"about_ca_system_score_gemma":0.00071411376,"threshold_uncertainty_score":0.08004713},"labels":[],"label_agreement":null},{"id":"W2789862492","doi":"10.1002/2017jb014966","title":"Catalog of Offshore Seismicity in Cascadia: Insights Into the Regional Distribution of Microseismicity and its Relation to Subduction Processes","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation of Sri Lanka; National Science Foundation","keywords":"Induced seismicity; Geology; Seismology; Subduction; Intraplate earthquake; Submarine pipeline; Seismometer; Triple junction; Pacific Plate; Deformation (meteorology); Tectonics; Oceanography","score_opus":0.0384170504282442,"score_gpt":0.3082508591527469,"score_spread":0.2698338087245027,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2789862492","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98387975,0.00033096672,0.00034955953,0.000045189514,0.000005035659,0.00002846704,0.012023298,0.00014177259,0.0031958423],"genre_scores_gemma":[0.97589207,0.00056816725,0.0006219193,0.0000133579615,0.000013199869,0.000053898188,0.02159057,0.000039988085,0.0012068339],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99966943,0.000023492788,0.00004944928,0.00008053047,0.000113633774,0.00006340084],"domain_scores_gemma":[0.99784625,0.00018195702,0.0006804196,0.00023395917,0.00063703593,0.0004204231],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003729476,0.0004699254,0.00037093836,0.008716805,0.0005380215,0.0005843298,0.00034528348,0.00020475216,0.0016678991],"category_scores_gemma":[0.0012518538,0.00023711857,0.00030980105,0.008004891,0.00027163333,0.00027286573,0.0011174567,0.0001641288,0.00046170113],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004484039,0.000015919397,0.98328364,0.000085085216,0.000057742986,0.00019041062,0.00065861875,0.00076361344,0.0026143973,0.00007871438,0.0011191812,0.011087821],"study_design_scores_gemma":[0.0000017721342,0.000009860163,0.99813473,0.000008140645,0.0000083501955,0.00004750265,0.00018526734,0.00020078442,0.00011293359,0.000018335364,0.0012684092,0.000003898675],"about_ca_topic_score_codex":0.062153365,"about_ca_topic_score_gemma":0.10745181,"teacher_disagreement_score":0.062153365,"about_ca_system_score_codex":0.0006312901,"about_ca_system_score_gemma":0.0008944333,"threshold_uncertainty_score":0.1235832},"labels":[],"label_agreement":null},{"id":"W2789876573","doi":"10.1002/2017jb014826","title":"Collisional Processes in the Crust of the Northern Tien Shan Inferred From Velocity and Attenuation Tomography Studies","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Institute of Population and Public Health; Russian Science Foundation; King Saud University; Russian Foundation for Basic Research","keywords":"Geology; Crust; Seismology; Kazakh; Attenuation; Shield; Seismic velocity; Anomaly (physics); Geophysics; Petrology","score_opus":0.06027908682772871,"score_gpt":0.3395020878383974,"score_spread":0.2792230010106687,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2789876573","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99948764,0.000024470099,0.00019097494,0.0000050339286,3.2853833e-7,0.000001610606,0.0000497333,0.00000694345,0.00023325816],"genre_scores_gemma":[0.9997441,0.000019292605,0.00011769239,5.7417355e-7,2.5883017e-7,8.486658e-7,0.00007214825,7.564671e-7,0.000044326698],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999434,0.000009769914,0.000005627725,0.000015939315,0.000011464945,0.000013837728],"domain_scores_gemma":[0.99984694,0.000025962645,0.000066899585,0.000021522845,0.000022243037,0.000016456876],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019261279,0.00022475705,0.00011234364,0.00062711484,0.00027990152,0.0005030732,0.00025507304,0.00012692534,0.0009973762],"category_scores_gemma":[0.00086119026,0.00016669395,0.0001563515,0.00081838307,0.0002231592,0.0003690469,0.00046628213,0.000109085864,0.00010412215],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000066802975,0.0000178572,0.9634531,0.0000184123,0.000039625113,0.000294158,0.00051112287,0.021561876,0.0038396239,0.00022413644,0.000066521156,0.009906794],"study_design_scores_gemma":[0.00000798222,0.000028441555,0.94425327,0.000010669947,0.00002030135,0.00013042752,0.00043002964,0.05391591,0.00068282685,0.0001696894,0.00034235013,0.000008207283],"about_ca_topic_score_codex":0.04733519,"about_ca_topic_score_gemma":0.05282663,"teacher_disagreement_score":0.04733519,"about_ca_system_score_codex":0.0005556891,"about_ca_system_score_gemma":0.00046712052,"threshold_uncertainty_score":0.09411931},"labels":[],"label_agreement":null},{"id":"W2790068703","doi":"10.1002/2017jb014606","title":"Poisson's Ratio and Auxetic Properties of Natural Rocks","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":116,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Bedford Institute of Oceanography; Polytechnique Montréal","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Quartz; Geology; Auxetics; Mineralogy; Coesite; Metamorphic rock; Poisson's ratio; Anorthite; Feldspar; Igneous rock; Siltstone; Isotropy; Mineral; Geochemistry; Petrology; Composite material; Materials science; Poisson distribution; Structural basin; Geomorphology","score_opus":0.04642425826704634,"score_gpt":0.3059357819474928,"score_spread":0.2595115236804465,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2790068703","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9907211,0.0007632097,0.0042582266,0.000015352305,0.0000057147704,0.000011300903,0.00034478382,0.000058066777,0.0038223497],"genre_scores_gemma":[0.9984518,0.000110210975,0.00091341144,0.0000029744422,0.00000387415,0.0000067177148,0.00018117974,0.000009566491,0.00032020273],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99965906,0.000038715043,0.00002882347,0.000075244214,0.00017172088,0.000026374437],"domain_scores_gemma":[0.9992648,0.00030641688,0.00019381836,0.000046848076,0.00015512998,0.000033067463],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039892094,0.00018172765,0.00013637336,0.0018832164,0.00016271127,0.0003521335,0.00040243551,0.00015352902,0.0013853282],"category_scores_gemma":[0.0014919867,0.00015903483,0.0001099643,0.00056170276,0.0003729325,0.0003827833,0.00024592408,0.000102681406,0.00023477203],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036810705,0.000051975316,0.23142864,0.00026423475,0.0001120301,0.00092014304,0.00039372648,0.007939073,0.71606344,0.004458267,0.000368476,0.037632022],"study_design_scores_gemma":[0.00001652289,0.00019755508,0.60935205,0.000022103848,0.000042344083,0.00394114,0.000517758,0.024546709,0.35265303,0.0029155472,0.005740943,0.000054349934],"about_ca_topic_score_codex":0.0004268564,"about_ca_topic_score_gemma":0.0003216576,"teacher_disagreement_score":0.0018832164,"about_ca_system_score_codex":0.00018248211,"about_ca_system_score_gemma":0.0000809637,"threshold_uncertainty_score":0.0046343803},"labels":[],"label_agreement":null},{"id":"W2790692559","doi":"10.1002/2017jb014921","title":"The Role of Recycled Oceanic Crust in the Generation of Alkaline A‐Type Granites","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Lakehead University","funders":"Youth Innovation Promotion Association; Youth Innovation Promotion Association of the Chinese Academy of Sciences; National Natural Science Foundation of China","keywords":"Geology; Subduction; Oceanic crust; Crust; Geochemistry; Mantle (geology); Intraplate earthquake; Adakite; Protolith; Zircon; Craton; Lithosphere; Partial melting; Paleontology; Tectonics","score_opus":0.0625706584644797,"score_gpt":0.32425426467315166,"score_spread":0.2616836062086719,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2790692559","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99889475,0.000171877,0.00026211166,0.000015411915,0.0000021805777,0.000003867686,0.000036411373,0.000017575765,0.00059580937],"genre_scores_gemma":[0.99897707,0.000104294166,0.00035598953,0.000007564185,0.000001524192,0.0000022131967,0.000055641114,0.000006694873,0.0004889794],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998982,0.0000055684154,0.000011212405,0.00003379424,0.000018321049,0.000032912627],"domain_scores_gemma":[0.9998431,0.000013119013,0.000043262262,0.000030446063,0.000035527362,0.000034559245],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020033467,0.0003403033,0.00023738663,0.00088092266,0.00063154736,0.000991803,0.0004466041,0.00037955111,0.0008771226],"category_scores_gemma":[0.00022927902,0.00030251275,0.0003418566,0.00038588422,0.0006021417,0.0003407659,0.0007471289,0.00023889724,0.00018453508],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040581194,0.000039834915,0.26947984,0.00017625642,0.00014934884,0.0012761605,0.00047809354,0.001581864,0.7082764,0.0017123849,0.00006273598,0.01636132],"study_design_scores_gemma":[0.000062278035,0.0001911569,0.8748306,0.000036249075,0.00015062989,0.0014195676,0.0012144387,0.0036351585,0.11290675,0.0012594452,0.0042533227,0.000040495266],"about_ca_topic_score_codex":0.0066973986,"about_ca_topic_score_gemma":0.007927903,"teacher_disagreement_score":0.0066973986,"about_ca_system_score_codex":0.0005882005,"about_ca_system_score_gemma":0.0006362897,"threshold_uncertainty_score":0.01331681},"labels":[],"label_agreement":null},{"id":"W2790953978","doi":"10.1002/2017jb015025","title":"Pressure and Stress Prediction in the Nankai Accretionary Prism: A Critical State Soil Mechanics Porosity‐Based Approach","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"","keywords":"Accretionary wedge; Geology; Porosity; Wedge (geometry); Pore water pressure; Shear (geology); Overburden pressure; Effective stress; Shear stress; Shearing (physics); Décollement; Differential stress; Stress (linguistics); Prism; Geotechnical engineering; Mineralogy; Mechanics; Subduction; Petrology; Materials science; Seismology; Geometry; Composite material; Deformation (meteorology); Optics; Tectonics","score_opus":0.039191433163419324,"score_gpt":0.3129041564054361,"score_spread":0.2737127232420168,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2790953978","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98123115,0.00006811882,0.01605215,0.00009045612,0.0000059790314,0.00001715571,0.00016424942,0.0000949597,0.0022757652],"genre_scores_gemma":[0.99893755,0.000019872976,0.00091254554,0.000004404098,0.0000014035872,0.0000042913,0.000041277668,0.0000033583722,0.000075237316],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999008,0.000016730777,0.000006825655,0.000023017437,0.000031040177,0.00002161383],"domain_scores_gemma":[0.9996662,0.00010030848,0.000062943785,0.000025663461,0.00010117826,0.000043776003],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029575234,0.00039130752,0.00032118475,0.00086568936,0.00044175438,0.0008576015,0.0012374877,0.0007156132,0.0006903184],"category_scores_gemma":[0.0012110827,0.00054901827,0.0004713507,0.0005181652,0.00073944964,0.0005911227,0.00058029825,0.00042370296,0.0001259202],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000045092493,0.000041192845,0.04742547,0.000029094832,0.00003206921,0.0001681108,0.000044717057,0.9425883,0.0035133867,0.0014722822,0.000101413905,0.0045389268],"study_design_scores_gemma":[0.000006951194,0.000018599258,0.0100556705,0.0000054561847,0.000004814974,0.000019915611,0.000023140594,0.9883359,0.0006844412,0.00078285893,0.00005332058,0.000008950878],"about_ca_topic_score_codex":0.032768562,"about_ca_topic_score_gemma":0.018743558,"teacher_disagreement_score":0.032768562,"about_ca_system_score_codex":0.0013292213,"about_ca_system_score_gemma":0.0014762812,"threshold_uncertainty_score":0.065155625},"labels":[],"label_agreement":null},{"id":"W2791424489","doi":"10.1002/2017jb014633","title":"Shear Modulus Dispersion in Cracked and Fluid‐Saturated Quartzites: Experimental Observations and Modeling","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Australian Research Council; Natural Sciences and Engineering Research Council of Canada; Australian National University; University of Alberta","keywords":"Saturation (graph theory); Shear (geology); Shear modulus; Porosity; Mineralogy; Materials science; Bulk modulus; Dispersion (optics); Composite material; Moduli; Elastic modulus; Geotechnical engineering; Geology; Optics","score_opus":0.08063912494904445,"score_gpt":0.3446936720364523,"score_spread":0.26405454708740783,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2791424489","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9945943,0.00004200534,0.004841155,0.0000128677575,9.0670034e-7,0.00000618502,0.00008816423,0.00004775392,0.00036665273],"genre_scores_gemma":[0.9987244,0.00002791901,0.0011055054,9.5162966e-7,6.366884e-7,0.000006116877,0.00004223431,0.0000036056892,0.00008866307],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993277,0.0000061882897,0.000005344345,0.000024779754,0.000023472188,0.000007437202],"domain_scores_gemma":[0.99986136,0.00006686076,0.000028811439,0.000017020373,0.000019910656,0.000005948707],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018799736,0.0002215148,0.00015770881,0.00029093758,0.00012538426,0.0001945002,0.00038958696,0.00029006708,0.0007089174],"category_scores_gemma":[0.000427575,0.00017753323,0.00013323376,0.0002608653,0.0003961684,0.00031435286,0.00016270195,0.00020847103,0.00008844332],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026731513,0.00014259716,0.021542609,0.00013460049,0.00002166689,0.00020556894,0.00021514183,0.09636776,0.87202585,0.0006831064,0.00009113398,0.008302707],"study_design_scores_gemma":[0.000033353914,0.00017335555,0.032548238,0.000008935573,0.000016041844,0.00009219557,0.00007496641,0.7010614,0.26519582,0.00034193907,0.0004312832,0.000022511573],"about_ca_topic_score_codex":0.0027239928,"about_ca_topic_score_gemma":0.0020614846,"teacher_disagreement_score":0.0027239928,"about_ca_system_score_codex":0.00030494863,"about_ca_system_score_gemma":0.00012118742,"threshold_uncertainty_score":0.005416274},"labels":[],"label_agreement":null},{"id":"W2792042872","doi":"10.1002/2017jb014546","title":"Mantle Lithosphere Rheology, Vertical Tectonics, and the Exhumation of (U)HP Rocks","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Türkiye Bilimsel ve Teknolojik Araştırma Kurumu","keywords":"Geology; Lithosphere; Subduction; Mantle (geology); Collision zone; Crustal recycling; Continental crust; Metamorphic rock; Crust; Terrane; Eclogitization; Petrology; Continental collision; Geochemistry; Geophysics; Tectonics; Oceanic crust; Seismology","score_opus":0.025087646342665186,"score_gpt":0.2949715445302824,"score_spread":0.2698838981876172,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2792042872","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986051,0.000030000918,0.0004218135,0.000026930917,0.0000016134065,0.0000018390798,0.0001307923,0.000018229443,0.00076362205],"genre_scores_gemma":[0.9997003,0.000015617343,0.00009533948,0.0000019435142,4.473703e-7,0.0000018619643,0.00004522982,0.0000036223264,0.00013556173],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.999962,0.000007680127,0.000003960976,0.000011419492,0.0000044047774,0.000010553057],"domain_scores_gemma":[0.99989355,0.00003819006,0.000028816927,0.00001534056,0.000013088132,0.000010999387],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012417349,0.00024145508,0.00016448286,0.00035542727,0.0002688917,0.0006270189,0.00030922593,0.00038181586,0.0014160306],"category_scores_gemma":[0.0005223137,0.0002558693,0.00031862865,0.0002843528,0.00029769124,0.00037860218,0.00033842484,0.00018423179,0.00013129106],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014964346,0.00004886687,0.15397911,0.000043533448,0.000104755396,0.00020556031,0.00008511186,0.8262018,0.013467334,0.0010130526,0.00013871986,0.004562521],"study_design_scores_gemma":[0.00004258571,0.00006227493,0.12805985,0.00001586295,0.00005533652,0.00009508643,0.00012303948,0.86523384,0.005434633,0.00043026844,0.00042728972,0.000020017033],"about_ca_topic_score_codex":0.029273678,"about_ca_topic_score_gemma":0.014005391,"teacher_disagreement_score":0.029273678,"about_ca_system_score_codex":0.000684366,"about_ca_system_score_gemma":0.0003045163,"threshold_uncertainty_score":0.058206618},"labels":[],"label_agreement":null},{"id":"W2793768150","doi":"10.1002/2017jb014524","title":"Migration Imaging of the Java Subduction Zones","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Slab; Subduction; Classification of discontinuities; Seismology; Discontinuity (linguistics); Trench; Transition zone; Mantle (geology); Underplating; Petrology; Geophysics; Tectonics","score_opus":0.03966884684266202,"score_gpt":0.3224649870142029,"score_spread":0.28279614017154087,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2793768150","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99697626,0.00006188376,0.0012030083,0.00002092304,0.0000043586633,0.0000068230233,0.00033203137,0.00008417065,0.0013105634],"genre_scores_gemma":[0.9966871,0.000056538393,0.0025877177,0.000007907616,0.0000032980452,0.0000039043907,0.0002774977,0.000012524064,0.00036342893],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999615,0.0000021393055,0.0000024083201,0.000012649624,0.000008966634,0.0000124335975],"domain_scores_gemma":[0.99993014,0.000005004119,0.000020513815,0.000004900783,0.000023093819,0.000016350703],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009148039,0.00025286738,0.000116383424,0.0010446531,0.00022604717,0.00030168757,0.00024314452,0.0001569834,0.00080224796],"category_scores_gemma":[0.00014870909,0.00012883145,0.00011609855,0.0006277697,0.00011842255,0.00017387689,0.00038407344,0.00016142662,0.00016883972],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048247125,0.00012076055,0.28262207,0.00011207084,0.00006839929,0.0005505113,0.0009127402,0.003771884,0.64074564,0.0004224827,0.000554173,0.06963687],"study_design_scores_gemma":[0.000029403285,0.000083953375,0.9604389,0.00001916557,0.000046919817,0.00031391424,0.00058004895,0.012507353,0.024079643,0.0001560536,0.0017215926,0.000023015558],"about_ca_topic_score_codex":0.011893591,"about_ca_topic_score_gemma":0.022527635,"teacher_disagreement_score":0.011893591,"about_ca_system_score_codex":0.0002245435,"about_ca_system_score_gemma":0.00023324123,"threshold_uncertainty_score":0.023648739},"labels":[],"label_agreement":null},{"id":"W2794878008","doi":"10.1002/2017jb015059","title":"Along‐Trench Structural Variations of the Subducting Juan de Fuca Plate From Multichannel Seismic Reflection Imaging","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Science Foundation","keywords":"Geology; Subduction; Seismology; Trench; Convergent boundary; Crust; Oceanic crust; Seafloor spreading; Slip (aerodynamics); Slab; Episodic tremor and slip; Mantle (geology); Receiver function; Slab window; Plate tectonics; Geophysics; Lithosphere; Tectonics","score_opus":0.04747210796864953,"score_gpt":0.3405989400635845,"score_spread":0.29312683209493495,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2794878008","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99855334,0.000032851844,0.00015503448,0.00000647267,0.0000019973832,0.00000301679,0.00020843494,0.000027741038,0.0010111408],"genre_scores_gemma":[0.9988362,0.000025922798,0.00049552304,0.0000033840654,0.0000033624153,0.00000340182,0.00028184525,0.0000058965534,0.0003444936],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992573,0.0000034281088,0.0000027194715,0.000025360147,0.000022600289,0.000020048463],"domain_scores_gemma":[0.99987113,0.000013341227,0.000043945365,0.000013610601,0.00003768149,0.000020209942],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014457824,0.00040709588,0.00015745788,0.0010799792,0.00022386776,0.0003439281,0.00022000227,0.0002632318,0.0010666547],"category_scores_gemma":[0.0002686434,0.00018689194,0.0001745222,0.0005945839,0.00018230594,0.00014490812,0.0002420673,0.00014546547,0.00018785633],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000295178,0.000087896326,0.7090218,0.00008832884,0.00015098455,0.0006473823,0.001335354,0.005068145,0.2386216,0.00009776524,0.0005021576,0.044083398],"study_design_scores_gemma":[0.0000025038432,0.000019720641,0.99659413,0.0000038869744,0.000010832806,0.00009009926,0.00014107027,0.0013452877,0.0014638159,0.000007770536,0.00031520726,0.0000057021107],"about_ca_topic_score_codex":0.022481231,"about_ca_topic_score_gemma":0.05496697,"teacher_disagreement_score":0.022481231,"about_ca_system_score_codex":0.00029354435,"about_ca_system_score_gemma":0.00025902336,"threshold_uncertainty_score":0.04470074},"labels":[],"label_agreement":null},{"id":"W2795257045","doi":"10.1002/2017jb014770","title":"Deformation of the Pacific/North America Plate Boundary at Queen Charlotte Fault: The Possible Role of Rheology","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Plate tectonics; Pacific Plate; North American Plate; Seismology; Convergent boundary; Terrane; Transform fault; Lithosphere; Boundary current; Thrust fault; Geodesy; Fault (geology); Oceanic crust; Subduction; Oceanography; Tectonics; Ocean current","score_opus":0.016157389714391086,"score_gpt":0.26236258673130547,"score_spread":0.24620519701691437,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2795257045","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99808025,0.00007020127,0.00008300844,0.000050893294,0.0000036081917,0.0000043012674,0.00008495788,0.000014556719,0.00160825],"genre_scores_gemma":[0.9997141,0.000022469345,0.000053730408,0.0000047398494,0.000001129494,0.0000010844145,0.000050479764,0.0000019942222,0.00015040107],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993443,0.0000068469762,0.0000046114023,0.000022374235,0.000015383792,0.000016349153],"domain_scores_gemma":[0.9997807,0.00002335366,0.000060187074,0.000011973676,0.000077476034,0.00004636544],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001365329,0.00018569082,0.00021833905,0.0010647669,0.0006346324,0.00093247695,0.00030734402,0.00038148154,0.0015099648],"category_scores_gemma":[0.0004915349,0.00018009823,0.00010719368,0.00048806387,0.0005376829,0.00034252554,0.00031630357,0.00019424631,0.0001906413],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022347787,0.00004639951,0.9339269,0.00006163126,0.0000472866,0.001010091,0.0006674951,0.002711831,0.050353628,0.00036692663,0.00044812023,0.01013632],"study_design_scores_gemma":[0.000003626563,0.000011710922,0.99494165,0.0000063074485,0.0000050399517,0.00006466753,0.00025009798,0.0035069385,0.0008900584,0.000042239626,0.00027110026,0.0000064689893],"about_ca_topic_score_codex":0.13086031,"about_ca_topic_score_gemma":0.099881805,"teacher_disagreement_score":0.8691397,"about_ca_system_score_codex":0.0012140914,"about_ca_system_score_gemma":0.00054022885,"threshold_uncertainty_score":0.26019728},"labels":[],"label_agreement":null},{"id":"W2801604508","doi":"10.1029/2017jb015282","title":"Continent‐Ocean Transition Across the Northeastern Nova Scotian Margin From a Dense Wide‐Angle Seismic Profile","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"Offshore Energy Research Association; U.S. Department of Energy","keywords":"Geology; Continental margin; Oceanic crust; Crust; Transition zone; Seismology; Seafloor spreading; Continental crust; Continental shelf; Mantle (geology); Rift; Subduction; Paleontology; Tectonics; Geophysics; Oceanography","score_opus":0.031809985161274416,"score_gpt":0.29738406714480636,"score_spread":0.26557408198353194,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2801604508","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99446684,0.00010757055,0.00013799508,0.000037957157,0.000005333802,0.000012469355,0.0019832111,0.000030583316,0.0032180862],"genre_scores_gemma":[0.9979766,0.00006849239,0.00018486544,0.000012482434,0.0000015907044,0.0000034967627,0.0009621745,0.000005425254,0.0007848644],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999503,0.0000020479226,0.000002662404,0.00001304353,0.000012616809,0.00001941774],"domain_scores_gemma":[0.99988186,0.0000052864534,0.000018126206,0.000006879663,0.00005668998,0.00003104634],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000061020026,0.00021436694,0.00010135507,0.0008405597,0.00046123637,0.0006672493,0.00020179109,0.00015804211,0.0018234937],"category_scores_gemma":[0.00019390654,0.000120915116,0.00019887589,0.00089451164,0.00019969484,0.00010311834,0.00035004545,0.00012560312,0.00020259077],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014954459,0.000040758758,0.9459262,0.00007280358,0.000103517385,0.0008599856,0.0005078492,0.018880723,0.014803922,0.00041131963,0.0017648527,0.016478483],"study_design_scores_gemma":[0.0000075092735,0.000007729453,0.99309266,0.000016706477,0.000011853674,0.00005097762,0.00031479553,0.0051173433,0.00022849764,0.000028861608,0.0011164516,0.000006557086],"about_ca_topic_score_codex":0.9370499,"about_ca_topic_score_gemma":0.9659814,"teacher_disagreement_score":0.062950075,"about_ca_system_score_codex":0.0029328456,"about_ca_system_score_gemma":0.003524487,"threshold_uncertainty_score":0.12664157},"labels":[],"label_agreement":null},{"id":"W2801743017","doi":"10.1029/2017jb015366","title":"Multiscale Insights Into Borehole Instabilities in High‐Porosity Sandstones","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Rock Mechanics and Modeling","field":"Engineering","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"Research Grants Council, University Grants Committee; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Borehole; Porosity; Failure mode and effects analysis; Geology; Stress path; Discrete element method; Compaction; Geotechnical engineering; Finite element method; Representative elementary volume; Stress (linguistics); Parametric statistics; Instability; Mechanics; Boundary value problem; Materials science; Shear (geology); Structural engineering; Composite material; Engineering; Petrology; Mathematics; Mathematical analysis","score_opus":0.028587379553133813,"score_gpt":0.31309254279336096,"score_spread":0.2845051632402271,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2801743017","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.82948726,0.00032065008,0.16669014,0.00017635513,0.000018975228,0.000030234085,0.000052309304,0.00014018042,0.0030838635],"genre_scores_gemma":[0.9954456,0.000046167428,0.004187957,0.000007703037,0.0000080119,0.0000086516275,0.000009733726,0.000008229249,0.00027787802],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998907,0.00002616472,0.0000062637664,0.000018832447,0.000032076525,0.000025910995],"domain_scores_gemma":[0.9997818,0.000051801744,0.00007516802,0.00001956472,0.00004087836,0.000030783856],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002486472,0.000297369,0.00033014736,0.0007413904,0.00034806877,0.0007175328,0.00046646374,0.00050208776,0.0007465517],"category_scores_gemma":[0.00055960316,0.0002490401,0.0004668937,0.00022319239,0.0009880295,0.0006311616,0.0007431032,0.00033925037,0.00007277892],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010279821,0.00011356002,0.017181972,0.0001229189,0.000100326804,0.0010873696,0.0004938139,0.7677631,0.1213198,0.08078299,0.00031409814,0.01061731],"study_design_scores_gemma":[0.000007322038,0.00002792497,0.0061332583,0.000005691966,0.0000065392533,0.00008382258,0.00007926193,0.98204654,0.0013471863,0.00998605,0.000263698,0.000012726834],"about_ca_topic_score_codex":0.0023278932,"about_ca_topic_score_gemma":0.0012952319,"teacher_disagreement_score":0.0023278932,"about_ca_system_score_codex":0.0004409832,"about_ca_system_score_gemma":0.00026961588,"threshold_uncertainty_score":0.004628718},"labels":[],"label_agreement":null},{"id":"W2804067255","doi":"10.1029/2017jb014155","title":"Necking of the Lithosphere: A Reappraisal of Basic Concepts With Thermo‐Mechanical Numerical Modeling","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"ExxonMobil Research and Engineering Company","keywords":"Necking; Geology; Lithosphere; Crust; Rift; Mantle (geology); Seismology; Petrology; Geophysics; Tectonics; Physics","score_opus":0.04214061179590726,"score_gpt":0.32308947112004843,"score_spread":0.28094885932414115,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2804067255","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5242979,0.007857578,0.43865502,0.002511154,0.00032914974,0.00014941553,0.000396776,0.00041841585,0.025384536],"genre_scores_gemma":[0.9625031,0.004282407,0.030953994,0.00011065943,0.00014166292,0.00010032968,0.00006967632,0.00010110559,0.0017369919],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998919,0.00003848971,0.000008375288,0.000014170799,0.000032362754,0.000014683228],"domain_scores_gemma":[0.99966776,0.00012763099,0.00006553179,0.00006770749,0.00004403555,0.000027259992],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045127084,0.00086865405,0.0006969981,0.00052355434,0.0004997386,0.0012435379,0.0014364772,0.0010868784,0.0009277964],"category_scores_gemma":[0.0012273939,0.0006160661,0.0011543509,0.00058148196,0.0018908033,0.0013650664,0.0010890975,0.00096145517,0.00013879738],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000024313364,0.000033456967,0.0021798457,0.000103295584,0.000036090732,0.00010552646,0.00014421597,0.95384705,0.0042574825,0.033766713,0.00016442845,0.0053374777],"study_design_scores_gemma":[0.000006236718,0.000012620271,0.0005283248,0.000016938597,0.0000054718394,0.000013795233,0.000014389178,0.9926103,0.00034492082,0.005898146,0.00053972064,0.000009125105],"about_ca_topic_score_codex":0.009589931,"about_ca_topic_score_gemma":0.0040481063,"teacher_disagreement_score":0.009589931,"about_ca_system_score_codex":0.0010908673,"about_ca_system_score_gemma":0.00068078365,"threshold_uncertainty_score":0.019068241},"labels":[],"label_agreement":null},{"id":"W2805797502","doi":"10.1029/2018jb015473","title":"Precambrian Plate Tectonics in Northern Hudson Bay: Evidence From <i>P</i> and <i>S</i> Wave Seismic Tomography and Analysis of Source Side Effects in Relative Arrival‐Time Data Sets","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Terrane; Geology; Precambrian; Lithosphere; Archean; Subduction; Seismology; Bay; Plate tectonics; Mantle (geology); Tectonics; Seismometer; Paleontology; Crust; Geophysics; Oceanography","score_opus":0.033324666137260185,"score_gpt":0.29970254532121193,"score_spread":0.2663778791839517,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2805797502","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983022,0.00010598814,0.00011234813,0.0000316527,0.0000032309865,0.000006834418,0.0007396734,0.000014346288,0.000683685],"genre_scores_gemma":[0.9986594,0.00007677745,0.00023783739,0.000009363653,0.0000024804658,0.000004501758,0.00079196115,0.0000045379225,0.00021305236],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99977463,0.000023948634,0.000018178616,0.00005906268,0.00006630541,0.000057827143],"domain_scores_gemma":[0.9992225,0.00009623477,0.0001714687,0.000073480005,0.0002972092,0.00013907428],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003016965,0.00026041476,0.0002319229,0.0015171388,0.00047681504,0.00096919725,0.00058836734,0.0002326145,0.0010179456],"category_scores_gemma":[0.0012979975,0.00028919504,0.00022165675,0.0024800876,0.00066701596,0.00026573677,0.000664841,0.00020277398,0.00015541568],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000057127756,0.00001621365,0.9878685,0.000026277903,0.000057437337,0.00015106294,0.000840781,0.0014400319,0.0021934442,0.0001589516,0.000311994,0.0068781236],"study_design_scores_gemma":[0.0000069847897,0.000009033121,0.9961119,0.000012368651,0.00001587895,0.000030385658,0.00078033144,0.0023361826,0.00022093931,0.00002660292,0.00044339025,0.0000060051857],"about_ca_topic_score_codex":0.85461295,"about_ca_topic_score_gemma":0.91925365,"teacher_disagreement_score":0.14538705,"about_ca_system_score_codex":0.003823601,"about_ca_system_score_gemma":0.0030191634,"threshold_uncertainty_score":0.2924865},"labels":[],"label_agreement":null},{"id":"W2806042432","doi":"10.1029/2017jb014894","title":"Shear Wave Tomography Beneath the United States Using a Joint Inversion of Surface and Body Waves","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"University of California, San Diego","keywords":"Geology; Lithosphere; Crust; Seismology; Seismic tomography; Mantle (geology); Geophysics; Surface wave; Tomography; Shear (geology); Seismic wave; Geodesy; Tectonics; Petrology; Physics","score_opus":0.058917526941551106,"score_gpt":0.3090273938239443,"score_spread":0.2501098668823932,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2806042432","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97862464,0.000044578795,0.01874305,0.00018782377,0.000012949191,0.000011484475,0.00026354258,0.00027581383,0.001836142],"genre_scores_gemma":[0.9951192,0.000021012764,0.0044567143,0.000008286306,0.0000036064355,0.0000045295706,0.0001253821,0.000010279885,0.0002510261],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999336,0.000016020202,0.0000040804184,0.000021859838,0.000012662005,0.000011818685],"domain_scores_gemma":[0.9998729,0.00002904298,0.000023438082,0.000019370704,0.000037332167,0.00001786488],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002467247,0.00040071725,0.00023878178,0.0003369647,0.0002820526,0.0006771932,0.00042496927,0.0004971604,0.00059538806],"category_scores_gemma":[0.0006394437,0.0004542815,0.0005136423,0.0005829853,0.0002517099,0.00055803324,0.00042357272,0.0003579473,0.00010228425],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007328167,0.00007050736,0.045349594,0.000012087907,0.00009709578,0.00010144031,0.00005613746,0.93313265,0.005835419,0.0011955701,0.0004830706,0.013593128],"study_design_scores_gemma":[0.00001072235,0.000011585169,0.0052030925,0.0000017728283,0.000013252779,0.000008775589,0.000011037517,0.9940696,0.00040179127,0.00017072992,0.00009222574,0.00000542665],"about_ca_topic_score_codex":0.110483356,"about_ca_topic_score_gemma":0.09426169,"teacher_disagreement_score":0.110483356,"about_ca_system_score_codex":0.00069882354,"about_ca_system_score_gemma":0.0012107954,"threshold_uncertainty_score":0.21968055},"labels":[],"label_agreement":null},{"id":"W2806792168","doi":"10.1029/2017jb015242","title":"Crustal Deformation Following Great Subduction Earthquakes Controlled by Earthquake Size and Mantle Rheology","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Subduction; Geology; Seismology; Mantle (geology); Viscoelasticity; Plate tectonics; Episodic tremor and slip; Interplate earthquake; Elastic-rebound theory; Geodetic datum; Earthquake rupture; Rheology; Crust; Geophysics; Geodesy; Fault (geology); Seismic gap; Tectonics","score_opus":0.0238578813710182,"score_gpt":0.3017235998731396,"score_spread":0.27786571850212144,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2806792168","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99953425,0.000010527689,0.00028771363,0.0000028846694,3.642353e-7,7.48263e-7,0.000035040062,0.000008454969,0.00011994134],"genre_scores_gemma":[0.99985695,0.0000054779243,0.0000718163,5.6081683e-7,2.0068681e-7,5.1416697e-7,0.000036582638,0.0000014866043,0.000026486696],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996686,0.000006032727,0.000002781969,0.00001084379,0.0000053220765,0.000008158615],"domain_scores_gemma":[0.999788,0.000058591155,0.00007168169,0.000033601205,0.000018833547,0.000029405173],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018093163,0.00017076706,0.00012621279,0.00041232814,0.00009185294,0.00029636003,0.00019097755,0.00018064083,0.0005093468],"category_scores_gemma":[0.00073474646,0.00015251902,0.00019614636,0.00023236337,0.00024569652,0.00018384293,0.00020768438,0.00012147666,0.00009936484],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047764336,0.00011264178,0.66253823,0.00004749821,0.00012485062,0.00038330758,0.0003833264,0.13773303,0.18281193,0.0007330555,0.00018013996,0.014474417],"study_design_scores_gemma":[0.000009181892,0.0000869051,0.8645971,0.000005958486,0.00001902017,0.00008235003,0.00008476736,0.12755229,0.0072898725,0.00013082218,0.00012739805,0.000014427632],"about_ca_topic_score_codex":0.0036078054,"about_ca_topic_score_gemma":0.0034627537,"teacher_disagreement_score":0.0036078054,"about_ca_system_score_codex":0.00021660353,"about_ca_system_score_gemma":0.00010191292,"threshold_uncertainty_score":0.007173598},"labels":[],"label_agreement":null},{"id":"W2808243099","doi":"10.1029/2018jb016001","title":"Particle Crushing of a Filled Fracture During Compression and Its Effect on Stress Wave Propagation","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Rock Mechanics and Modeling","field":"Engineering","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"China Scholarship Council; China Postdoctoral Science Foundation; Chinese Academy of Sciences; National Natural Science Foundation of China","keywords":"Materials science; Deformation (meteorology); Fracture (geology); Compression (physics); Composite material; Softening; Stress (linguistics); Comminution; Compressive strength; Fracture mechanics; Geotechnical engineering; Geology; Metallurgy","score_opus":0.028783295079017723,"score_gpt":0.31521114689819674,"score_spread":0.286427851819179,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2808243099","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999198,0.00006174611,0.00061555475,0.0000064364494,0.0000040657756,0.000002892764,0.000018689054,0.000014383735,0.000078295736],"genre_scores_gemma":[0.99969363,0.00002006481,0.00019139632,0.0000035411292,8.0084226e-7,0.000001700761,0.000013216501,0.0000015860428,0.000074041716],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989533,0.000008004293,0.0000066769135,0.0000163876,0.000048191196,0.000025437224],"domain_scores_gemma":[0.9996488,0.00013115331,0.00008509383,0.00002903212,0.00006362449,0.00004225833],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001566643,0.00021627005,0.00020712611,0.00023669055,0.00020148503,0.0001650132,0.000185021,0.00030652905,0.0006566904],"category_scores_gemma":[0.00042820314,0.00012060869,0.00022717543,0.00013219984,0.00029246995,0.00018192218,0.00015686579,0.00029772246,0.000051396568],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047460216,0.00007928457,0.011746108,0.00007113674,0.00002797562,0.000693506,0.00012795604,0.005397678,0.9733661,0.000054703032,0.00007639782,0.007884621],"study_design_scores_gemma":[0.000028053166,0.0016007464,0.16403078,0.000016996017,0.000043741875,0.0004977788,0.0003656388,0.0897548,0.74298537,0.00013497817,0.0005005262,0.00004051852],"about_ca_topic_score_codex":0.0017680832,"about_ca_topic_score_gemma":0.002096167,"teacher_disagreement_score":0.0017680832,"about_ca_system_score_codex":0.00015325667,"about_ca_system_score_gemma":0.00007814821,"threshold_uncertainty_score":0.0035156608},"labels":[],"label_agreement":null},{"id":"W2809750982","doi":"10.1029/2018jb015641","title":"Tongji‐Grace02s and Tongji‐Grace02k: High‐Precision Static GRACE‐Only Global Earth's Gravity Field Models Derived by Refined Data Processing Strategies","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Danmarks Tekniske Universitet; Chinese Academy of Sciences; State Key Laboratory of Geo-Information Engineering; National Natural Science Foundation of China; TU Graz, Internationale Beziehungen und Mobilitätsprogramme","keywords":"Accelerometer; Geopotential; Gravitational field; Geodesy; Gravitational acceleration; Calibration; Acceleration; Noise (video); Gravity of Earth; Polynomial; Orbit determination; Mathematics; Computer science; Satellite; Statistics; Physics; Geology; Mathematical analysis; Aerospace engineering; Engineering","score_opus":0.08610367856281079,"score_gpt":0.3661051760196522,"score_spread":0.28000149745684144,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2809750982","genre_codex":"empirical","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93424624,0.00019899831,0.04247205,0.00041157036,0.00009785363,0.00010490635,0.013779585,0.0028915922,0.0057971883],"genre_scores_gemma":[0.9581909,0.00010582451,0.02190792,0.00009057789,0.000028209817,0.00010206699,0.017475415,0.00036906876,0.001729886],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99976915,0.00004581547,0.000016972495,0.0000732871,0.000055732093,0.000039039547],"domain_scores_gemma":[0.9995937,0.000039828636,0.000058322563,0.00010706577,0.00016318126,0.000038067214],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009274543,0.00091764826,0.00050707144,0.00076951436,0.00031466494,0.00069423934,0.0010135536,0.0005835015,0.0014881209],"category_scores_gemma":[0.001368712,0.000442197,0.0011894233,0.0016419988,0.0003963947,0.00095013366,0.00057447015,0.0007509385,0.0007179849],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016850773,0.00010865969,0.037668675,0.000081048835,0.00026719924,0.00012205456,0.00009564835,0.9290277,0.0062817037,0.0014643286,0.0050018006,0.01971271],"study_design_scores_gemma":[0.000060124243,0.00001972794,0.02800131,0.0000065806385,0.000042984633,0.000016177773,0.000025538815,0.96867204,0.0012041763,0.0002497312,0.0016601167,0.000041415024],"about_ca_topic_score_codex":0.1317427,"about_ca_topic_score_gemma":0.087833434,"teacher_disagreement_score":0.1317427,"about_ca_system_score_codex":0.0009819944,"about_ca_system_score_gemma":0.002614281,"threshold_uncertainty_score":0.2619518},"labels":[],"label_agreement":null},{"id":"W2845257977","doi":"10.1029/2018jb015600","title":"The Elastic Properties of Clay in Shales","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Schlumberger (Canada)","funders":"","keywords":"Geomechanics; Anisotropy; Clay minerals; Geology; Shear modulus; Geotechnical engineering; Bulk modulus; Porosity; Elastic modulus; Stiffness; Shear (geology); Mineralogy; Permeability (electromagnetism); Materials science; Petrology; Composite material; Chemistry; Physics","score_opus":0.056951061645565466,"score_gpt":0.3194668736964606,"score_spread":0.26251581205089514,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2845257977","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988764,0.000042228094,0.000645061,0.00001342333,0.0000010275484,0.0000014319037,0.000028719689,0.0000057887005,0.0003858998],"genre_scores_gemma":[0.9996731,0.000014819059,0.00005852746,0.0000031391837,4.8171614e-7,6.681694e-7,0.00002292471,0.0000010055522,0.000225361],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999628,0.0000042122883,0.0000020290909,0.000011120585,0.00001015316,0.000009719899],"domain_scores_gemma":[0.99986446,0.000041512107,0.000033713623,0.0000096055865,0.0000293431,0.000021337852],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014025712,0.00015871171,0.00009786469,0.00045500373,0.00025422472,0.00028102644,0.00015495828,0.00022068547,0.0010257161],"category_scores_gemma":[0.00031643177,0.00013246166,0.000089105735,0.00014807987,0.0003905916,0.0003287441,0.00028674718,0.00014339789,0.00011327045],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00049024634,0.00014734307,0.094227865,0.00015424086,0.00007643913,0.00083372317,0.00036494623,0.24112242,0.64745677,0.003381556,0.0002797281,0.011464663],"study_design_scores_gemma":[0.00003712628,0.00024010442,0.18406329,0.000023281606,0.00003426714,0.00020843849,0.0006283988,0.7091825,0.10292838,0.0015808989,0.001020564,0.00005273393],"about_ca_topic_score_codex":0.0043487283,"about_ca_topic_score_gemma":0.0033216479,"teacher_disagreement_score":0.0043487283,"about_ca_system_score_codex":0.00022410334,"about_ca_system_score_gemma":0.00016226692,"threshold_uncertainty_score":0.008646846},"labels":[],"label_agreement":null},{"id":"W2851025245","doi":"10.1029/2018jb015581","title":"The<i>M</i>7 2016 Kumamoto, Japan, Earthquake: 3‐D Deformation Along the Fault and Within the Damage Zone Constrained From Differential Lidar Topography","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":122,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Southern California Earthquake Center; National Science Foundation","keywords":"Fault trace; Geology; Seismology; Fault (geology); Geodesy; Deformation (meteorology); Slip (aerodynamics); Echelon formation; Displacement (psychology)","score_opus":0.02265004269761835,"score_gpt":0.28125703748043757,"score_spread":0.25860699478281923,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2851025245","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981772,0.000033238677,0.00079078734,0.000027475717,0.0000033411136,0.0000035599426,0.00023687865,0.000026460837,0.0007011357],"genre_scores_gemma":[0.9984604,0.000030846786,0.0010473717,0.0000062377167,0.0000028571615,0.0000033935391,0.00033179866,0.000006019447,0.00011101405],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996686,0.0000033247834,0.0000026382795,0.000009804137,0.000009795193,0.0000076659535],"domain_scores_gemma":[0.999905,0.00000942951,0.0000326627,0.000014889042,0.000023275512,0.000014756643],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011180512,0.0001633318,0.00017425665,0.000308115,0.00019528272,0.00046055648,0.00017232967,0.00026163546,0.0005575186],"category_scores_gemma":[0.00033716182,0.00016864664,0.00014508812,0.0004532654,0.00019230852,0.00022954654,0.00032654472,0.00014959456,0.0001858506],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019324016,0.000112201196,0.73430747,0.00012933493,0.000112463975,0.0010036519,0.00064222753,0.0431055,0.14827947,0.0007965363,0.0022720767,0.069045775],"study_design_scores_gemma":[0.000010887724,0.000036875295,0.9320954,0.000015266705,0.000027497661,0.00014349945,0.0002757391,0.061359137,0.0048404844,0.00021309234,0.00095910893,0.000022882943],"about_ca_topic_score_codex":0.013216073,"about_ca_topic_score_gemma":0.031592693,"teacher_disagreement_score":0.013216073,"about_ca_system_score_codex":0.00026135275,"about_ca_system_score_gemma":0.00035461277,"threshold_uncertainty_score":0.026278317},"labels":[],"label_agreement":null},{"id":"W2880778462","doi":"10.1029/2018jb015655","title":"Using Drones and Miniaturized Instrumentation to Study Degassing at Turrialba and Masaya Volcanoes, Central America","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Volcano; Drone; Flux (metallurgy); Instrumentation (computer programming); Geology; Materials science; Seismology; Computer science; Biology","score_opus":0.03171131953861521,"score_gpt":0.33501807647006865,"score_spread":0.3033067569314534,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2880778462","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99865675,0.000047363337,0.00033636604,0.000014607973,0.0000045015486,0.000019436984,0.00016452427,0.000024907196,0.00073160225],"genre_scores_gemma":[0.9979804,0.000059946433,0.001371413,0.00002003608,0.000004928255,0.000025206748,0.00027004842,0.0000075474413,0.00026054573],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998808,0.000014111196,0.000005243443,0.000044151628,0.00003130037,0.000024373336],"domain_scores_gemma":[0.9998154,0.000026098607,0.00004401833,0.000020051722,0.00006107616,0.00003348444],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018578274,0.0004157325,0.00026160353,0.0009115777,0.00049424625,0.0004470277,0.00043506597,0.0002550497,0.00036971737],"category_scores_gemma":[0.00030569846,0.00016827656,0.0001793083,0.00061392697,0.00035304073,0.0004055672,0.00044806115,0.0002814799,0.000076232274],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00050449173,0.00037274367,0.8263284,0.00013288444,0.00022117632,0.0012121586,0.0023021006,0.011769525,0.12886202,0.000279789,0.00056884723,0.027445868],"study_design_scores_gemma":[0.00003559315,0.00031260872,0.96712846,0.000021413534,0.00006727034,0.00016405858,0.002038777,0.0167616,0.010623792,0.00007367578,0.002736114,0.000036653826],"about_ca_topic_score_codex":0.064150445,"about_ca_topic_score_gemma":0.16002426,"teacher_disagreement_score":0.064150445,"about_ca_system_score_codex":0.00090859784,"about_ca_system_score_gemma":0.00048811833,"threshold_uncertainty_score":0.12755412},"labels":[],"label_agreement":null},{"id":"W2883006360","doi":"10.1029/2017jb015132","title":"Infrasound Signal Detection and Back Azimuth Estimation Using Ground‐Coupled Airwaves on a Seismo‐Acoustic Sensor Pair","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Resources Canada; National Science Foundation","keywords":"Azimuth; Seismometer; Infrasound; Geology; Acoustics; Seismology; SIGNAL (programming language); Microphone; Microseism; Seismogram; Noise (video); Remote sensing; Geodesy; Computer science; Physics; Optics; Artificial intelligence","score_opus":0.044940190053129596,"score_gpt":0.31869939530059943,"score_spread":0.27375920524746983,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2883006360","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6083157,0.00009698594,0.38854057,0.00007831244,0.000060801165,0.000052009214,0.0002323381,0.0011058174,0.0015173916],"genre_scores_gemma":[0.7832997,0.000049436014,0.21510653,0.000035968933,0.000025774543,0.000040597068,0.00030508987,0.000043075335,0.0010937281],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99975497,0.00003175207,0.000009214737,0.00004977346,0.00013121717,0.000023156788],"domain_scores_gemma":[0.99964666,0.000098413526,0.000046410358,0.000057264013,0.0001220831,0.000029278463],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014913354,0.0004229233,0.0003272291,0.00059774483,0.00016414054,0.00033727227,0.0004669491,0.00037793774,0.0010780416],"category_scores_gemma":[0.00090403063,0.00024978752,0.0002873194,0.00043090628,0.00017500295,0.00037484316,0.0005315018,0.00035805686,0.00041127508],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00057267246,0.00017457655,0.019527515,0.00008189693,0.00015273447,0.0001923911,0.00015062532,0.042410187,0.56335604,0.00056237093,0.00076410593,0.37205493],"study_design_scores_gemma":[0.00008115547,0.00026548718,0.033176463,0.000011351313,0.00007990124,0.0001831326,0.000073462325,0.82342994,0.14040686,0.0003666596,0.0018677067,0.00005772198],"about_ca_topic_score_codex":0.0036421951,"about_ca_topic_score_gemma":0.0059824707,"teacher_disagreement_score":0.0036421951,"about_ca_system_score_codex":0.00016454278,"about_ca_system_score_gemma":0.00044202505,"threshold_uncertainty_score":0.007242024},"labels":[],"label_agreement":null},{"id":"W2883875668","doi":"10.1029/2018jb015545","title":"Controls on Mid‐ocean Ridge Normal Fault Seismicity Across Spreading Rates From Rate‐and‐State Friction Models","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Division of Earth Sciences; Division of Ocean Sciences; National Science Foundation","keywords":"Geology; Seismology; Seismic moment; Induced seismicity; Slip (aerodynamics); Ridge; Fault (geology); Tectonics; Seismic gap; Geodetic datum; Geodesy; Paleontology","score_opus":0.05216554651928905,"score_gpt":0.33673283381953956,"score_spread":0.2845672873002505,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2883875668","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.986981,0.00006942847,0.010082793,0.00011751208,0.000005305792,0.00002085766,0.00014640439,0.00004986791,0.0025268395],"genre_scores_gemma":[0.9995036,0.000021965434,0.00022475062,0.0000049741657,0.0000011188602,0.000004165249,0.00003787942,0.000006299831,0.00019530657],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998035,0.00006994851,0.000012322084,0.00003768764,0.00002917991,0.000047434096],"domain_scores_gemma":[0.99874854,0.0006680778,0.0002641708,0.00013706203,0.000081321654,0.00010081831],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009636097,0.0006074486,0.0005002231,0.00055142463,0.00024828216,0.0009447667,0.0008051574,0.0005081604,0.0014947135],"category_scores_gemma":[0.0036598449,0.00042087483,0.00077630667,0.0002821032,0.00058786874,0.0008101703,0.0006288167,0.0005466145,0.00011391124],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012984787,0.0000760517,0.020278756,0.00002946625,0.00007374994,0.00011225657,0.000062544044,0.95993346,0.009880435,0.0074119875,0.00015563522,0.001855823],"study_design_scores_gemma":[0.000010906655,0.000019974388,0.004992467,0.0000024823976,0.000012242724,0.000013938893,0.000010224312,0.9932637,0.00047714356,0.0011432997,0.00004535274,0.000008335192],"about_ca_topic_score_codex":0.013909906,"about_ca_topic_score_gemma":0.008110692,"teacher_disagreement_score":0.013909906,"about_ca_system_score_codex":0.000984088,"about_ca_system_score_gemma":0.0005479324,"threshold_uncertainty_score":0.027657866},"labels":[],"label_agreement":null},{"id":"W2883977859","doi":"10.1029/2018jb015992","title":"Paleomagnetism and Geochemistry of ~1144‐Ma Lamprophyre Dikes, Northwestern Ontario: Implications for the North American Polar Wander and Plate Velocities","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Lakehead University","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Geology; Dike; Apparent polar wander; Paleomagnetism; Geochemistry; Ultramafic rock; Rift; Mantle plume; Basalt; Outcrop; Geophysics; Seismology; Tectonics; Lithosphere","score_opus":0.02763427566962862,"score_gpt":0.27837427648445384,"score_spread":0.2507400008148252,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2883977859","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977035,0.00010132264,0.00004362473,0.000018242832,8.8167917e-7,0.0000030860795,0.00031191477,0.0000044112517,0.0018131412],"genre_scores_gemma":[0.9982363,0.00008787628,0.00010525712,0.0000064763567,9.983875e-7,0.0000031798024,0.00027710304,0.0000032533812,0.001279541],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999027,0.000003980037,0.00000442267,0.000021987264,0.00003652383,0.000030358313],"domain_scores_gemma":[0.999801,0.000010552807,0.00004289874,0.000007309019,0.00011074049,0.000027605687],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000085141575,0.00018673485,0.00018539643,0.0014136584,0.0013540464,0.00076963025,0.0002616841,0.0001710671,0.0016789688],"category_scores_gemma":[0.00031843793,0.00018306749,0.00011619689,0.0011780552,0.00051991333,0.00021107135,0.00037681186,0.00013207673,0.00018805599],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001609399,0.000009596244,0.9508968,0.000048437392,0.0000410476,0.00018036451,0.0019896885,0.00021386729,0.039003577,0.00011504664,0.00020053587,0.007140092],"study_design_scores_gemma":[0.0000015133922,0.0000054519933,0.99837494,0.0000036167548,0.00000623135,0.000027132128,0.00033918137,0.00006291269,0.00053787575,0.000010844921,0.0006278903,0.0000023519794],"about_ca_topic_score_codex":0.80536216,"about_ca_topic_score_gemma":0.93006706,"teacher_disagreement_score":0.19463784,"about_ca_system_score_codex":0.0051765586,"about_ca_system_score_gemma":0.0018521927,"threshold_uncertainty_score":0.39156818},"labels":[],"label_agreement":null},{"id":"W2884526877","doi":"10.1029/2017jb015417","title":"Structural Inheritance Control on Intraplate Present‐Day Deformation: GPS Strain Rate Variations in the Saint Lawrence Valley, Eastern Canada","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"Natural Resources Canada; Agence Nationale de la Recherche; Université Laval","keywords":"Intraplate earthquake; Strain rate; Lithosphere; Post-glacial rebound; Geology; Tectonics; Global Positioning System; Geodesy; Strain rate tensor; Induced seismicity; Seismology; Inheritance (genetic algorithm); Paleontology; Glacial period; Genetics","score_opus":0.03731815646045556,"score_gpt":0.2945067029427489,"score_spread":0.25718854648229333,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2884526877","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99736834,0.000059570855,0.0002418005,0.000048789523,0.000001303621,0.000004511357,0.0009737435,0.000019644962,0.0012821986],"genre_scores_gemma":[0.9991074,0.00002589045,0.0001338428,0.00000510636,6.1474185e-7,0.0000011930432,0.00041761526,0.0000029899627,0.00030535934],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99978024,0.0000152866,0.000008433742,0.000047506695,0.0000778334,0.00007064901],"domain_scores_gemma":[0.9992355,0.00009086314,0.000099535486,0.000041797262,0.00043730254,0.00009497443],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002441064,0.00023292768,0.00024446275,0.001000452,0.0009614002,0.0010768545,0.0006227722,0.00018138748,0.0010119929],"category_scores_gemma":[0.00091056863,0.00013791358,0.00021064452,0.0018855329,0.0006039646,0.00017583442,0.00040156292,0.0002342249,0.0000939219],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000091467446,0.000020128251,0.9746249,0.000020210036,0.00008263632,0.00014201073,0.0005782492,0.008929781,0.0029374307,0.0004897221,0.00073933887,0.0113442615],"study_design_scores_gemma":[0.0000031446034,0.0000043759537,0.9925833,0.0000054860693,0.000009750381,0.000014849389,0.0003654,0.0063107526,0.00022279173,0.00004405657,0.0004262566,0.000009919996],"about_ca_topic_score_codex":0.9877456,"about_ca_topic_score_gemma":0.9919784,"teacher_disagreement_score":0.012254417,"about_ca_system_score_codex":0.008791861,"about_ca_system_score_gemma":0.007783876,"threshold_uncertainty_score":0.063789725},"labels":[],"label_agreement":null},{"id":"W2886428601","doi":"10.1029/2017jb015039","title":"Surface Rupture Morphology and Vertical Slip Distribution of the 1959<b><i>M</i></b><sub><b><i>w</i></b></sub>7.2 Hebgen Lake (Montana) Earthquake From Airborne Lidar Topography","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Division of Earth Sciences; Natural Sciences and Engineering Research Council of Canada; Southern California Earthquake Center; National Science Foundation","keywords":"Fault scarp; Geology; Canyon; Slip (aerodynamics); Seismology; Fault (geology); Escarpment; Geodetic datum; Surface rupture; Paleoseismology; Geodesy; Geomorphology","score_opus":0.02155665216389295,"score_gpt":0.2703957479061825,"score_spread":0.24883909574228952,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2886428601","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999527,0.000015410453,0.00003906953,0.000004336718,2.9238237e-7,7.3795e-7,0.00013901334,0.0000043294535,0.00026991987],"genre_scores_gemma":[0.99952257,0.000008859175,0.00006225643,0.0000022192658,6.1063747e-7,7.2977457e-7,0.00028837693,0.0000010482229,0.00011333647],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996865,0.0000026367222,0.0000019008323,0.000010153219,0.000008988024,0.000007654117],"domain_scores_gemma":[0.9998833,0.000012548217,0.000038584018,0.0000066117705,0.00003531836,0.000023572038],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000630538,0.00006956057,0.00007729618,0.0005663877,0.00014847206,0.0002869282,0.00011483818,0.00019607416,0.0007700055],"category_scores_gemma":[0.00018267326,0.000072772404,0.00006443263,0.00042074083,0.00014491004,0.00013223337,0.00014484249,0.00006618985,0.00016773093],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011269042,0.000026802669,0.9621319,0.0000138060195,0.000026073621,0.00024709458,0.00036335914,0.0009818424,0.025528695,0.000052210118,0.0003136484,0.010201735],"study_design_scores_gemma":[6.678496e-7,0.000006915613,0.9992481,7.4412054e-7,0.0000012945577,0.000031373507,0.00006759502,0.00035529915,0.00022483528,0.0000039386805,0.000058104466,0.0000010959603],"about_ca_topic_score_codex":0.019720964,"about_ca_topic_score_gemma":0.040914938,"teacher_disagreement_score":0.019720964,"about_ca_system_score_codex":0.00032045497,"about_ca_system_score_gemma":0.00006537499,"threshold_uncertainty_score":0.039212346},"labels":[],"label_agreement":null},{"id":"W2887308933","doi":"10.1029/2018jb015620","title":"Geodetically Inferred Locking State of the Cascadia Megathrust Based on a Viscoelastic Earth Model","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":112,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Viscoelasticity; Geodetic datum; Geodesy; Seismology; Slip (aerodynamics); Earth model; Subduction; Creep; Tectonics; Engineering","score_opus":0.04737862865242928,"score_gpt":0.3204798114179897,"score_spread":0.2731011827655604,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2887308933","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98777974,0.00004055262,0.009320212,0.00008299181,0.000005856473,0.000003905283,0.0002722581,0.00022366182,0.002270708],"genre_scores_gemma":[0.9989316,0.000023308272,0.0006465792,0.000004133878,9.506532e-7,0.0000018835289,0.00013767568,0.000011717263,0.00024209451],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99996495,0.0000052388555,0.0000027285485,0.000013695251,0.000005926869,0.000007466238],"domain_scores_gemma":[0.9999006,0.000016025295,0.000019598534,0.000024448338,0.000020494163,0.000018908957],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011850785,0.0003904196,0.00017099714,0.00054822315,0.000211201,0.00046061884,0.0004155748,0.00043827656,0.0012166568],"category_scores_gemma":[0.0005641602,0.00022681445,0.00027140472,0.0003847547,0.00026176072,0.00033078188,0.0002850224,0.00024291419,0.00020781571],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006873688,0.000035642268,0.09449623,0.000025860341,0.000057135498,0.00024083798,0.00009945753,0.88131565,0.014398606,0.001516863,0.00036836666,0.007376607],"study_design_scores_gemma":[0.000011414026,0.00002083091,0.03988153,0.0000065659224,0.000015147396,0.00003066086,0.000043334927,0.95800817,0.0011137453,0.00052398397,0.00033201382,0.000012578103],"about_ca_topic_score_codex":0.03417964,"about_ca_topic_score_gemma":0.023763495,"teacher_disagreement_score":0.03417964,"about_ca_system_score_codex":0.0006360324,"about_ca_system_score_gemma":0.0004326818,"threshold_uncertainty_score":0.067961335},"labels":[],"label_agreement":null},{"id":"W2888271949","doi":"10.1029/2018jb015768","title":"Frictional Mechanics of Slow Earthquakes","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":100,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"Pennsylvania State University; National Science Foundation","keywords":"Slip (aerodynamics); Mechanics; Instability; Geology; Rheology; Slip line field; Episodic tremor and slip; Seismology; Physics; Tectonics; Subduction; Shear (geology); Petrology","score_opus":0.05153245529519993,"score_gpt":0.32499826954208794,"score_spread":0.273465814246888,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2888271949","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9969283,0.00011064198,0.0017852812,0.000017002712,0.000003691539,0.000008037766,0.000038175054,0.000022086144,0.0010867948],"genre_scores_gemma":[0.99983823,0.000020045793,0.000053253036,0.0000015586396,6.775553e-7,0.0000017483876,0.000007207496,8.8321343e-7,0.00007638744],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999527,0.0000068626796,0.0000035056119,0.000011776595,0.000014381385,0.0000108136055],"domain_scores_gemma":[0.9998282,0.00004440782,0.000055986085,0.000023948227,0.00002127957,0.000026014703],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011219151,0.00016490436,0.00020778837,0.0003102867,0.0001579213,0.00030156795,0.00013897364,0.00014550528,0.0011888326],"category_scores_gemma":[0.0003783393,0.00010258587,0.000082784485,0.00008819176,0.0003660275,0.00018712749,0.00026766036,0.00015333005,0.00011311437],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00054060214,0.0001938072,0.038027808,0.00016051758,0.00005450066,0.00079634215,0.00034104715,0.057601314,0.87650675,0.005067952,0.00042586727,0.020283422],"study_design_scores_gemma":[0.00011271504,0.0024855235,0.31817642,0.00003706028,0.000051363728,0.0010571531,0.00058036146,0.4762953,0.18546465,0.012027927,0.0036069588,0.000104511644],"about_ca_topic_score_codex":0.00044765542,"about_ca_topic_score_gemma":0.00030528253,"teacher_disagreement_score":0.0011888326,"about_ca_system_score_codex":0.00018789628,"about_ca_system_score_gemma":0.00009529334,"threshold_uncertainty_score":0.0039770603},"labels":[],"label_agreement":null},{"id":"W2889126220","doi":"10.1029/2018jb015740","title":"Inferences of Mantle Viscosity Based on Ice Age Data Sets: The Bias in Radial Viscosity Profiles Due to the Neglect of Laterally Heterogeneous Viscosity Structure","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Division of Earth Sciences; Harvard University","keywords":"Post-glacial rebound; Mantle (geology); Geology; Lithosphere; Viscosity; Geophysics; Geopotential; Geodesy; Physics; Glacial period; Thermodynamics; Seismology; Tectonics","score_opus":0.0889560900454589,"score_gpt":0.3577850746601862,"score_spread":0.2688289846147273,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2889126220","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98311114,0.0000646314,0.015437432,0.00006108228,0.000007902665,0.000010699179,0.0004817152,0.00019767554,0.0006277355],"genre_scores_gemma":[0.99337244,0.000031811305,0.0057191397,0.000013385507,0.000005797127,0.0000062009667,0.000773351,0.000034872275,0.000042991385],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996897,0.00011746812,0.000028117596,0.000065729015,0.000062440595,0.000036587335],"domain_scores_gemma":[0.9983512,0.00093354547,0.00022426703,0.00023518252,0.0001872642,0.00006863215],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015277838,0.00039434398,0.00028441273,0.0006456981,0.00020440789,0.00092382735,0.00043357257,0.00042709368,0.0004600471],"category_scores_gemma":[0.0075126966,0.00034192475,0.0005730409,0.00042840544,0.00037597102,0.00056052214,0.000499402,0.0003981941,0.00011201491],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048522354,0.00013354888,0.18323858,0.000097817676,0.0004840551,0.00012732038,0.00022136331,0.71508604,0.058269847,0.0020685769,0.0003878084,0.039399743],"study_design_scores_gemma":[0.000058346082,0.000052142816,0.10183755,0.000029809724,0.000056251578,0.000055017994,0.000057762434,0.8797177,0.016563695,0.0010413546,0.00048187192,0.000048467664],"about_ca_topic_score_codex":0.012574702,"about_ca_topic_score_gemma":0.01079413,"teacher_disagreement_score":0.012574702,"about_ca_system_score_codex":0.00035550504,"about_ca_system_score_gemma":0.00046796078,"threshold_uncertainty_score":0.025003016},"labels":[],"label_agreement":null},{"id":"W2889144529","doi":"10.1029/2018jb015771","title":"Seismic Imaging of the North American Midcontinent Rift Using <i>S</i>‐to‐<i>P</i> Receiver Functions","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"H2020 European Research Council; Natural Environment Research Council; Sight Research UK; National Science Foundation","keywords":"Geology; Rift; Lithosphere; Underplating; Seismology; Discontinuity (linguistics); Tectonics; Fibrous joint; Gravity anomaly; Paleontology","score_opus":0.027605030819423466,"score_gpt":0.3028696462038336,"score_spread":0.27526461538441016,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2889144529","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97872627,0.00020576926,0.0061515626,0.00032904593,0.000020422138,0.00002695216,0.002671127,0.0011152695,0.010753571],"genre_scores_gemma":[0.98312634,0.00011667866,0.012996334,0.00008802934,0.000016534403,0.000016337828,0.0016506375,0.00005126652,0.0019377078],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99994254,0.0000045933084,0.0000013231439,0.000016537984,0.000020586702,0.000014438476],"domain_scores_gemma":[0.99985623,0.000014247356,0.000020695174,0.00000914526,0.000073407784,0.000026136937],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000120459394,0.0002485434,0.000110183566,0.0007723538,0.000246304,0.00034433856,0.00024802994,0.00021547987,0.0018574708],"category_scores_gemma":[0.00021148995,0.00017311577,0.00011940737,0.0004900189,0.00010707884,0.00015535596,0.00019563701,0.00022030977,0.00037067838],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000520629,0.00028311642,0.35338715,0.00015114582,0.00018361915,0.0008137738,0.0012979226,0.013916271,0.41712812,0.0010176471,0.014619651,0.19668093],"study_design_scores_gemma":[0.00004765292,0.000109325854,0.9216124,0.000040671406,0.00006865974,0.00033335236,0.00042824485,0.052986562,0.016017236,0.0002376315,0.008080365,0.000037999176],"about_ca_topic_score_codex":0.029729081,"about_ca_topic_score_gemma":0.10372213,"teacher_disagreement_score":0.029729081,"about_ca_system_score_codex":0.00028856573,"about_ca_system_score_gemma":0.00049115013,"threshold_uncertainty_score":0.059112072},"labels":[],"label_agreement":null},{"id":"W2890316842","doi":"10.1029/2018jb015638","title":"Smoothing of Fault Slip Surfaces by Scale‐Invariant Wear","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Geological Society of America","keywords":"Slip (aerodynamics); Geometry; Geology; Asperity (geotechnical engineering); Slip line field; Surface finish; Scaling; Smoothing; Surface roughness; Materials science; Geotechnical engineering; Shear (geology); Composite material; Petrology; Physics; Mathematics","score_opus":0.037766970490561505,"score_gpt":0.3202534218637282,"score_spread":0.2824864513731667,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2890316842","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99819916,0.000032057524,0.0014636825,0.0000054460347,0.0000010055866,0.000003440935,0.000058773723,0.000042085885,0.00019448163],"genre_scores_gemma":[0.9995223,0.000006833543,0.00036696254,9.541391e-7,7.830165e-7,0.0000012752093,0.000045765777,0.000004671186,0.000050351435],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985886,0.000014481932,0.0000054534776,0.00004244207,0.00004833806,0.000030290408],"domain_scores_gemma":[0.9992987,0.00018413825,0.00023754226,0.000113716706,0.00012274501,0.00004323079],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015637581,0.00014516257,0.00031017815,0.0011664819,0.00020504482,0.00041100997,0.00016989297,0.00015797687,0.00053756934],"category_scores_gemma":[0.0010264169,0.00019413872,0.00019179653,0.0005292181,0.0003633179,0.00023500023,0.00026209035,0.00013412272,0.00006422417],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048611435,0.00012414051,0.51491123,0.00013385295,0.00018846092,0.0005474918,0.0009544103,0.033317856,0.39169073,0.00076580636,0.00064705656,0.056232825],"study_design_scores_gemma":[0.000004829147,0.000052296244,0.93655807,0.0000044269045,0.000013725405,0.00013482884,0.00012247084,0.052320875,0.010164664,0.0002865733,0.00031745105,0.00001977929],"about_ca_topic_score_codex":0.0022729512,"about_ca_topic_score_gemma":0.003248584,"teacher_disagreement_score":0.0022729512,"about_ca_system_score_codex":0.00032125428,"about_ca_system_score_gemma":0.000107649306,"threshold_uncertainty_score":0.0045194626},"labels":[],"label_agreement":null},{"id":"W2890617922","doi":"10.1029/2018jb016192","title":"Geometric Complexity of Earthquake Rupture Surfaces Preserved in Pseudotachylyte Networks","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University; Niagara College; McGill University","funders":"","keywords":"Seismology; Geology; Sinistral and dextral; Earthquake rupture; Fault plane; Rake; Slip (aerodynamics); Shear (geology); Fault (geology); Rake angle; Seismic gap; Perpendicular; Geometry; Petrology; Engineering","score_opus":0.08782578788538091,"score_gpt":0.33472939956115694,"score_spread":0.246903611675776,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2890617922","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983664,0.000029655788,0.0006339348,0.00001079289,6.3706995e-7,0.0000021363307,0.000110026696,0.000010967631,0.0008354771],"genre_scores_gemma":[0.9994574,0.000018460842,0.00022433231,0.0000015632119,0.0000017407668,0.0000020144334,0.00020050516,0.0000034190446,0.00009045512],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998735,0.000018367498,0.000008468259,0.00004274658,0.000031050044,0.00002583879],"domain_scores_gemma":[0.99923,0.00021567274,0.00031156075,0.00006058982,0.00011261933,0.00006953471],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011818193,0.000096252734,0.00021959841,0.002123451,0.00023342812,0.0009841955,0.0002175716,0.00018644465,0.0017612409],"category_scores_gemma":[0.0013873787,0.00014645825,0.00010982263,0.0010448522,0.0005252956,0.0006042842,0.00054949726,0.00013720777,0.00017414751],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005795664,0.00007541412,0.8396455,0.00015272867,0.00012548151,0.0009412181,0.0016884586,0.028771583,0.07572586,0.010641661,0.00076122937,0.040891286],"study_design_scores_gemma":[0.000009258939,0.00006611966,0.96038735,0.000011075995,0.000018278966,0.000705958,0.0008436112,0.030821236,0.0021185358,0.003809969,0.0011937271,0.000014797605],"about_ca_topic_score_codex":0.0009758394,"about_ca_topic_score_gemma":0.0011177735,"teacher_disagreement_score":0.002123451,"about_ca_system_score_codex":0.00029032578,"about_ca_system_score_gemma":0.00008736459,"threshold_uncertainty_score":0.005891919},"labels":[],"label_agreement":null},{"id":"W2895695694","doi":"10.1029/2018jb015626","title":"Muon Tomography Applied to a Dense Uranium Deposit at the McArthur River Mine","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Particle Detector Development and Performance","field":"Physics and Astronomy","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Saskatchewan; Geoscience BC","funders":"","keywords":"Uranium; Geology; Tomography; Muon; Nuclear physics; Physics","score_opus":0.025016389402503267,"score_gpt":0.31419128004463437,"score_spread":0.2891748906421311,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2895695694","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9959747,0.00006206669,0.0020661154,0.000040365234,0.0000026007315,0.000026770396,0.00011630759,0.000052589832,0.0016585533],"genre_scores_gemma":[0.99651957,0.000052272946,0.0031049435,0.000008835489,0.0000015160207,0.000004973519,0.000039143008,0.0000070685874,0.00026155348],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998499,0.00001785534,0.000006603005,0.00001985898,0.0000811129,0.000024606083],"domain_scores_gemma":[0.99974245,0.000075483644,0.00004233179,0.000024501373,0.00009681909,0.000018520976],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002496923,0.00022492128,0.00025042158,0.0008519134,0.0005898395,0.00048637242,0.0004029242,0.00027540408,0.0006758651],"category_scores_gemma":[0.00076676905,0.00020206528,0.00011186452,0.00089835434,0.00036396203,0.00024301797,0.0005245021,0.00018655937,0.00010151486],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006197034,0.00012355935,0.23889856,0.0001684036,0.000072664996,0.0059003374,0.0027654772,0.01491346,0.67759603,0.00091296877,0.00042843434,0.057600267],"study_design_scores_gemma":[0.00007457331,0.0005674553,0.75569683,0.00006176493,0.00008782644,0.0044390014,0.0027309358,0.05025681,0.18079974,0.00043054027,0.004791502,0.00006303805],"about_ca_topic_score_codex":0.06331593,"about_ca_topic_score_gemma":0.13189377,"teacher_disagreement_score":0.06331593,"about_ca_system_score_codex":0.0007298298,"about_ca_system_score_gemma":0.0007321663,"threshold_uncertainty_score":0.12589478},"labels":[],"label_agreement":null},{"id":"W2896395469","doi":"10.1029/2018jb016240","title":"Renewed Posteruptive Uplift Following the 2011–2012 Rhyolitic Eruption of Cordón Caulle (Southern Andes, Chile): Evidence for Transient Episodes of Magma Reservoir Recharge During 2012–2018","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Geology; Sill; Magma; Volcano; Interferometric synthetic aperture radar; Seismology; Induced seismicity; Petrology; Synthetic aperture radar","score_opus":0.09905648980286537,"score_gpt":0.3632131987235892,"score_spread":0.26415670892072385,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2896395469","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985226,0.00010312668,0.000042950007,0.000053697346,0.000005753024,0.0000048867396,0.00028737856,0.000018828501,0.0009608756],"genre_scores_gemma":[0.9994523,0.00004720114,0.000038983097,0.000011087466,0.000009933454,0.0000042765155,0.00027346064,0.000003889492,0.00015894375],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999093,0.000005576752,0.000006763049,0.00003134709,0.000017614568,0.00002939388],"domain_scores_gemma":[0.99952257,0.000059841852,0.00018340845,0.000035816724,0.00011643318,0.00008198967],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024481775,0.00021123099,0.00019969484,0.0008469958,0.00043844015,0.00055422995,0.00040420145,0.00043660213,0.0014279208],"category_scores_gemma":[0.0007961763,0.0001489586,0.0001814797,0.00060722284,0.00035756038,0.00030497304,0.0004675631,0.00028162537,0.00022363332],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029346207,0.000058720692,0.9714239,0.000093353665,0.000077584526,0.00093540235,0.0009332403,0.00056945015,0.015620162,0.000092691604,0.0006716713,0.009230364],"study_design_scores_gemma":[0.0000035249498,0.0000107026,0.99877125,0.000005672638,0.000009355329,0.000042273245,0.00015602063,0.00050169276,0.00021360094,0.000009727724,0.00027314818,0.0000031331408],"about_ca_topic_score_codex":0.051692057,"about_ca_topic_score_gemma":0.055878058,"teacher_disagreement_score":0.051692057,"about_ca_system_score_codex":0.0008219727,"about_ca_system_score_gemma":0.00046982645,"threshold_uncertainty_score":0.10278237},"labels":[],"label_agreement":null},{"id":"W2898144743","doi":"10.1029/2018jb015880","title":"The Effects of Hydrate on the Strength and Stiffness of Some Sands","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":97,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Hydrate; Clathrate hydrate; Seabed; Cementation (geology); Sediment; Geology; Stiffness; Particle size; Saturation (graph theory); Dissociation (chemistry); Instability; Mineralogy; Geotechnical engineering; Materials science; Chemistry; Composite material; Geomorphology; Cement; Mechanics","score_opus":0.0164153387908374,"score_gpt":0.29929972584782594,"score_spread":0.28288438705698854,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2898144743","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99947125,0.00004904534,0.00017867831,0.000005100533,0.0000011152722,0.000004261094,0.00004441204,0.0000080077825,0.00023833671],"genre_scores_gemma":[0.999348,0.000031623884,0.00026993843,0.000005281661,6.7087467e-7,0.0000033348335,0.000054701646,0.0000041584844,0.00028227593],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998192,0.000025944822,0.00001778391,0.000023519287,0.00008361691,0.000029883133],"domain_scores_gemma":[0.9993358,0.00022602956,0.00014306838,0.000058759226,0.00014773407,0.000088610555],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025593833,0.00020705385,0.00014651005,0.0003996283,0.00025049585,0.0002660651,0.00022084313,0.0001727538,0.0011847663],"category_scores_gemma":[0.00060264237,0.00018135807,0.00020595673,0.0001927265,0.0004298499,0.00022956797,0.00028425385,0.0002541152,0.00011031266],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041946594,0.000039755803,0.009690988,0.00004858679,0.000031371157,0.00010293517,0.00006698464,0.0015892157,0.98402494,0.000031333126,0.000023347686,0.003931023],"study_design_scores_gemma":[0.0000073412452,0.00092046574,0.080459036,0.000004215393,0.000022620974,0.00012550087,0.00012568891,0.0030495026,0.91477025,0.000026670928,0.00047701786,0.000011681506],"about_ca_topic_score_codex":0.0033216733,"about_ca_topic_score_gemma":0.0059439195,"teacher_disagreement_score":0.0033216733,"about_ca_system_score_codex":0.00044001677,"about_ca_system_score_gemma":0.000181789,"threshold_uncertainty_score":0.0066046715},"labels":[],"label_agreement":null},{"id":"W2899458936","doi":"10.1029/2018jb016506","title":"On the Physics of the Inner‐Core Wobble; Corrections to “Dynamics of the Inner‐Core Wobble Under Mantle‐Inner‐Core Gravitational Interactions” by B. F. Chao","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Research Institute for Sustainable Humanosphere, Kyoto University; University of Science and Technology of China; Ministry of Science and Technology, Taiwan; National Aeronautics and Space Administration; National Science Foundation","keywords":"Speed wobble; Inner core; Hydrostatic equilibrium; Mantle (geology); Physics; Geodesy; Quadrupole; Earth model; Gravitation; Geophysics; Geology; Classical mechanics; Astronomy; Quantum mechanics","score_opus":0.08184214748902914,"score_gpt":0.33918810273559935,"score_spread":0.2573459552465702,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2899458936","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.4109026,0.019345429,0.45336035,0.03842071,0.023159485,0.00015143676,0.0015027196,0.0044333823,0.048723884],"genre_scores_gemma":[0.9552477,0.004098243,0.024475183,0.0012371652,0.0022524598,0.000040072493,0.0003380098,0.001273089,0.011038127],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99983144,0.000032531785,0.000008213746,0.000046795496,0.000065504406,0.00001538391],"domain_scores_gemma":[0.99960595,0.00008042842,0.00009467165,0.000064891065,0.00011284224,0.000041257415],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00070009107,0.0006788584,0.00028838037,0.00080624374,0.00053205027,0.00094400544,0.0008048157,0.0007359122,0.0018306596],"category_scores_gemma":[0.0041100504,0.00033415464,0.00037855434,0.0005087015,0.000886681,0.0010508592,0.0011854973,0.0014121083,0.00049383065],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027175664,0.000064544016,0.030074308,0.000580573,0.00016103528,0.0019966422,0.00096165296,0.1788828,0.06832484,0.44844517,0.07586896,0.19436775],"study_design_scores_gemma":[0.00005651696,0.000041563446,0.0404343,0.00013265519,0.000065483335,0.00052040024,0.000106009335,0.7174429,0.020996016,0.11051398,0.10951991,0.00017027285],"about_ca_topic_score_codex":0.009005582,"about_ca_topic_score_gemma":0.003832254,"teacher_disagreement_score":0.009005582,"about_ca_system_score_codex":0.00083859125,"about_ca_system_score_gemma":0.0008449632,"threshold_uncertainty_score":0.017906308},"labels":[],"label_agreement":null},{"id":"W2899615550","doi":"10.1029/2018jb016555","title":"Probabilistic Surface Heat Flow Estimates Assimilating Paleoclimate History: New Implications for the Thermochemical Structure of Ireland","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Irish Research Council","keywords":"Laurentia; Geology; Radiogenic nuclide; Paleoclimatology; Crust; Geophysics; Lithosphere; Terrane; Paleontology; Climate change; Mantle (geology); Tectonics; Oceanography","score_opus":0.057448604425390216,"score_gpt":0.31497572518793787,"score_spread":0.25752712076254763,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2899615550","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9424722,0.00019262198,0.054438826,0.00027460937,0.000013248737,0.000012121141,0.000498205,0.00025319657,0.0018449628],"genre_scores_gemma":[0.9930714,0.00003675103,0.006516504,0.000014554533,0.0000073175083,0.000004280882,0.00021159006,0.000021898817,0.000115709154],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9994325,0.00017781873,0.00004904662,0.00017708562,0.00010542647,0.00005802287],"domain_scores_gemma":[0.9973302,0.0012714508,0.0005496202,0.000310629,0.00046607704,0.00007199574],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001980727,0.0003591702,0.0002659809,0.0010289052,0.00022165994,0.0012752777,0.0006399027,0.00033799346,0.00041538881],"category_scores_gemma":[0.009385995,0.0003592832,0.00052381965,0.0006350054,0.0006337282,0.0009813873,0.0009157922,0.00044742099,0.00010622245],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001593399,0.000018853103,0.29567248,0.000046637942,0.00020630799,0.00006225819,0.00024173169,0.65560645,0.0070633404,0.0024776575,0.00034513924,0.038099848],"study_design_scores_gemma":[0.000018616212,0.000027338625,0.12731014,0.000031888354,0.000031181404,0.000042950014,0.000119025695,0.8656556,0.0021068475,0.0036515591,0.00093339605,0.000071534116],"about_ca_topic_score_codex":0.033419997,"about_ca_topic_score_gemma":0.03104757,"teacher_disagreement_score":0.033419997,"about_ca_system_score_codex":0.001142011,"about_ca_system_score_gemma":0.0009220918,"threshold_uncertainty_score":0.06645095},"labels":[],"label_agreement":null},{"id":"W2900858623","doi":"10.1029/2018jb016472","title":"Modeling High Stress Drops, Scaling, Interaction, and Irregularity of Repeating Earthquake Sequences Near Parkfield","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"U.S. Geological Survey; Southern California Earthquake Center; National Science Foundation","keywords":"Scaling; Seismic moment; Slip (aerodynamics); Seismology; Moment (physics); Geology; Stress (linguistics); Scaling law; Induced seismicity; Fault (geology); Physics; Mathematics; Geometry; Classical mechanics; Thermodynamics","score_opus":0.051730927662836206,"score_gpt":0.33612787483698364,"score_spread":0.28439694717414743,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2900858623","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99106276,0.000031197153,0.008145187,0.000053719257,0.000004506398,0.000008571008,0.000055005443,0.00004630041,0.0005927575],"genre_scores_gemma":[0.9989492,0.000016526927,0.00080339843,0.0000032796254,0.0000034232296,0.000004258194,0.000026549047,0.00000538545,0.00018799155],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999337,0.0000117029385,0.0000038134583,0.000026934773,0.000006981809,0.000016765653],"domain_scores_gemma":[0.9996891,0.000113954084,0.00008697424,0.000029653733,0.000029360739,0.000050958755],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018422652,0.0003869145,0.00033145712,0.0005296976,0.00025618883,0.00069043686,0.0009070565,0.00088299706,0.0006832917],"category_scores_gemma":[0.0009940616,0.0003905549,0.00044946364,0.0003359011,0.00045908793,0.00054902554,0.00038609502,0.00036820452,0.00007571283],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000022654307,0.00005451293,0.013716175,0.000009420621,0.000024124285,0.00011140912,0.00003434417,0.9815409,0.0018652048,0.0009372897,0.000073884825,0.0016101175],"study_design_scores_gemma":[0.000002717969,0.000007375028,0.001335214,4.8166726e-7,0.000002957088,0.000005397739,0.000006097459,0.9984131,0.00008346826,0.00012160798,0.00001980591,0.0000017304561],"about_ca_topic_score_codex":0.027956856,"about_ca_topic_score_gemma":0.01560626,"teacher_disagreement_score":0.027956856,"about_ca_system_score_codex":0.00068404,"about_ca_system_score_gemma":0.00041517644,"threshold_uncertainty_score":0.055588245},"labels":[],"label_agreement":null},{"id":"W2901238718","doi":"10.1029/2018jb016630","title":"Short‐Time Geodetic Determination of Aquifer Storage Coefficient in Taiwan","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"Ministry of Science and Technology, Taiwan; Central Geological Survey, Ministry of Economic Affairs","keywords":"Gravimeter; Geodetic datum; Aquifer; Geology; Geodesy; Groundwater; Subsidence; Hydrogeology; Gravimetry; Geotechnical engineering; Geomorphology; Geophysics","score_opus":0.049651701769996316,"score_gpt":0.33125901431234356,"score_spread":0.2816073125423472,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2901238718","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99921703,0.000011146733,0.0004466859,0.000011481764,8.631228e-7,0.0000018405578,0.00010753494,0.000026399684,0.00017699072],"genre_scores_gemma":[0.9996973,0.0000045065617,0.00015652836,0.0000012122758,3.0767896e-7,0.0000017909664,0.00009781246,0.0000026691023,0.00003785466],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999074,0.0000118555145,0.000008345821,0.000033675708,0.000018334586,0.000020435324],"domain_scores_gemma":[0.9996904,0.00007593357,0.00006295485,0.000043670316,0.000091838265,0.000035161167],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032799682,0.00026691472,0.00022412962,0.00079083117,0.00025437362,0.00039318932,0.00048761538,0.00031663186,0.0005059844],"category_scores_gemma":[0.0005966745,0.00020182534,0.00028808604,0.00088287547,0.00022178362,0.00045282836,0.00026278544,0.00016020724,0.00008700427],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013909335,0.00012533458,0.83074194,0.000054197808,0.00009227115,0.0005674348,0.0002647411,0.12609212,0.02408393,0.00030133806,0.0005512792,0.01698632],"study_design_scores_gemma":[0.00003446747,0.00010246684,0.51547265,0.000012129049,0.00004534441,0.000086001,0.00033933876,0.47341058,0.009798532,0.00019646241,0.0004502809,0.000051812905],"about_ca_topic_score_codex":0.04582486,"about_ca_topic_score_gemma":0.04674918,"teacher_disagreement_score":0.04582486,"about_ca_system_score_codex":0.00067116617,"about_ca_system_score_gemma":0.00055542856,"threshold_uncertainty_score":0.09111625},"labels":[],"label_agreement":null},{"id":"W2901604451","doi":"10.1029/2018jb016559","title":"Weak and Slow, Strong and Fast: How Shear Zones Evolve in a Dry Continental Crust (Musgrave Ranges, Central Australia)","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"Università degli Studi di Padova; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung","keywords":"Geology; Shear zone; Mylonite; Mafic; Crust; Continental crust; Gneiss; Geochemistry; Shear (geology); Quartz; Petrology; Metamorphic rock; Seismology; Tectonics; Paleontology","score_opus":0.056614086045254704,"score_gpt":0.3216680148280227,"score_spread":0.265053928782768,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2901604451","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993954,0.00008931121,0.0000299342,0.000010371773,4.3291044e-7,0.00000225319,0.000042381347,0.0000018703006,0.00042807075],"genre_scores_gemma":[0.9994174,0.000059970607,0.000071918075,0.000008988924,6.2222034e-7,0.0000019377846,0.000062550396,0.000003153282,0.00037334455],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984884,0.000020476888,0.000008021037,0.00005506512,0.000027349724,0.00004033925],"domain_scores_gemma":[0.9997799,0.000022135511,0.000063312604,0.000011096285,0.00006471644,0.00005890768],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000237544,0.00018392305,0.00018017947,0.0014789947,0.0006426797,0.0010526318,0.000372591,0.00034934186,0.0011768367],"category_scores_gemma":[0.0006880406,0.00026976655,0.00013869126,0.0010557375,0.0010857007,0.00039142653,0.0009787999,0.00022601227,0.00018098892],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016348781,0.000029022856,0.91349447,0.00010243752,0.00012232533,0.00040565513,0.011662346,0.0007784082,0.05397152,0.0005779554,0.00022170377,0.018470723],"study_design_scores_gemma":[6.267203e-7,0.000011311652,0.99853146,0.0000043667155,0.0000036874571,0.000032881748,0.00079852797,0.00017220245,0.00012552894,0.00003390101,0.00028305655,0.0000024950011],"about_ca_topic_score_codex":0.0773406,"about_ca_topic_score_gemma":0.13913165,"teacher_disagreement_score":0.0773406,"about_ca_system_score_codex":0.0012431572,"about_ca_system_score_gemma":0.000383355,"threshold_uncertainty_score":0.15378088},"labels":[],"label_agreement":null},{"id":"W2902134171","doi":"10.1029/2018jb016151","title":"Subseafloor Temperature Variations Influenced by Variations in Bottom Water Temperature and Pressure: New High Resolution Observations and Implications","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"Woods Hole Oceanographic Institution; National Science Foundation","keywords":"Seafloor spreading; Geology; Accretionary wedge; Sediment; Clathrate hydrate; Ridge; Seawater; Geothermal gradient; Prism; Methane; Pore water pressure; Oceanography; Geomorphology; Petrology; Geophysics; Seismology; Hydrate; Tectonics; Paleontology; Subduction","score_opus":0.01884396762338718,"score_gpt":0.28893519559277264,"score_spread":0.27009122796938545,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2902134171","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99339265,0.00019065489,0.0037829909,0.000043808024,0.000015381172,0.000012461756,0.0007734184,0.00014592345,0.0016427047],"genre_scores_gemma":[0.99282455,0.00009124876,0.0058455486,0.000020292815,0.000022023274,0.000010638977,0.0006466229,0.00002225807,0.0005168027],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998229,0.000016080034,0.0000059402128,0.000067349996,0.000061935105,0.000025805939],"domain_scores_gemma":[0.9997098,0.000044113523,0.00004894484,0.000046569534,0.00007996265,0.000070588605],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032394784,0.00026291073,0.00024836528,0.000506826,0.0003534573,0.0005472017,0.00046767338,0.0003530047,0.00050045486],"category_scores_gemma":[0.00042552626,0.00027330185,0.00020692755,0.00058960036,0.00027740872,0.00039996923,0.00036988995,0.00045369292,0.00012253897],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039190994,0.00019088137,0.65232337,0.00012310894,0.00015867314,0.0005386992,0.00066586985,0.0039579594,0.29524946,0.00013031549,0.00078440766,0.045485336],"study_design_scores_gemma":[0.000015782567,0.00005609372,0.97735673,0.000007638198,0.00004150083,0.00018415115,0.00010677415,0.0087141255,0.012067563,0.000049906066,0.0013761731,0.000023564515],"about_ca_topic_score_codex":0.018527778,"about_ca_topic_score_gemma":0.048480082,"teacher_disagreement_score":0.018527778,"about_ca_system_score_codex":0.00042811234,"about_ca_system_score_gemma":0.0002319333,"threshold_uncertainty_score":0.036839843},"labels":[],"label_agreement":null},{"id":"W2902279869","doi":"10.1029/2018jb015719","title":"The Lithospheric Structure of the Solonker Suture Zone and Adjacent Areas: Crustal Anisotropy Revealed by a High‐Resolution Magnetotelluric Study","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"China Geological Survey; National Natural Science Foundation of China","keywords":"Geology; Magnetotellurics; Anisotropy; Lithosphere; Fibrous joint; Subduction; Electrical resistivity and conductivity; Craton; Geophysics; Conductivity; Fold (higher-order function); Seismology; Petrology; Tectonics","score_opus":0.014511488906988923,"score_gpt":0.28970363770952845,"score_spread":0.2751921488025395,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2902279869","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995728,0.000040182193,0.00006660856,0.0000048504885,7.387338e-7,0.0000011274544,0.000042194795,0.000003628284,0.00026784284],"genre_scores_gemma":[0.99970716,0.000027680071,0.00009994591,0.0000026949876,0.0000020354014,0.0000010803133,0.00008191305,0.0000017049546,0.0000757853],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995136,0.000006374673,0.0000038659473,0.0000151810455,0.000010420655,0.000012867017],"domain_scores_gemma":[0.999933,0.000010715683,0.00001835465,0.000007897693,0.000015903208,0.000014128281],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001363774,0.00025070252,0.00022210465,0.00082454464,0.0002873076,0.00051658513,0.0001662972,0.0002508615,0.000603941],"category_scores_gemma":[0.00019789192,0.00015366946,0.00016811554,0.0007156132,0.0002499345,0.00024485931,0.00035080645,0.00013167434,0.00010915683],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002649749,0.00007618275,0.83466214,0.000062668965,0.0001800006,0.001235701,0.0013454116,0.0015539895,0.1415802,0.00021264424,0.00012784761,0.018698227],"study_design_scores_gemma":[0.0000036070787,0.000019889212,0.99736905,0.0000034492723,0.000013198375,0.0000977538,0.00027950646,0.0010354175,0.0009529307,0.00002636393,0.00019474307,0.0000040843556],"about_ca_topic_score_codex":0.006033788,"about_ca_topic_score_gemma":0.012554547,"teacher_disagreement_score":0.006033788,"about_ca_system_score_codex":0.00020052043,"about_ca_system_score_gemma":0.00017469685,"threshold_uncertainty_score":0.011997342},"labels":[],"label_agreement":null},{"id":"W2904915630","doi":"10.1029/2018jb016199","title":"Thermal, Deformation, and Degassing Remote Sensing Time Series (CE 2000–2017) at the 47 most Active Volcanoes in Latin America: Implications for Volcanic Systems","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Earthquake Detection and Analysis","field":"Earth and Planetary Sciences","cited_by":102,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Comisión Nacional de Investigación Científica y Tecnológica; Natural Environment Research Council; Canadian Space Agency; Agenzia Spaziale Italiana; Sight Research UK; Leverhulme Trust; European Space Agency; National Aeronautics and Space Administration; U.S. Geological Survey; NERC Environmental Bioinformatics Centre; National Science Foundation","keywords":"Volcano; Geology; Volcanism; Satellite; Seismology; Magma; Earth science; Lava; Tectonics","score_opus":0.033962960338998247,"score_gpt":0.3060763205992533,"score_spread":0.27211336026025507,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2904915630","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99167836,0.0008659834,0.0002607024,0.00062952866,0.000022451577,0.0000120783825,0.00506006,0.000039708022,0.0014311236],"genre_scores_gemma":[0.9922321,0.0005217848,0.000631662,0.00008938765,0.000039599767,0.000024008625,0.0061713723,0.000020268446,0.00026984932],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997819,0.000047354428,0.0000231522,0.00006143015,0.000026906551,0.00005924776],"domain_scores_gemma":[0.99900705,0.00020935819,0.0003225584,0.00008202087,0.00026104218,0.00011789759],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008183581,0.00032980953,0.00027256075,0.0015840704,0.00023051398,0.00096917554,0.0003654529,0.00031000224,0.0010448949],"category_scores_gemma":[0.001800273,0.00008874517,0.00044818188,0.0020492598,0.00031968358,0.00058348506,0.00050253235,0.00024016223,0.00015466349],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006615509,0.000041878124,0.981913,0.00005958522,0.0000938604,0.00008598842,0.00021096127,0.0020750451,0.0018437203,0.00010819701,0.001231069,0.012270656],"study_design_scores_gemma":[0.000006109275,0.000014982772,0.9949504,0.000039809114,0.000028026894,0.00002579832,0.0007315668,0.0022194285,0.00029393664,0.00006026971,0.0016222906,0.0000073886363],"about_ca_topic_score_codex":0.06746405,"about_ca_topic_score_gemma":0.067359686,"teacher_disagreement_score":0.06746405,"about_ca_system_score_codex":0.0008948974,"about_ca_system_score_gemma":0.00048559072,"threshold_uncertainty_score":0.13414276},"labels":[],"label_agreement":null},{"id":"W2905132918","doi":"10.1029/2018jb016697","title":"Mountain Building Orogeny in Precollision Hot Backarcs: North American Cordillera, India‐Tibet, and Grenville Province","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Orogeny; Geology; Lithosphere; Crust; Continental crust; Collision zone; Continental collision; Subduction; Metamorphism; Collision; Continental margin; Mountain formation; Oceanic crust; Earth science; Petrology; Seismology; Tectonics; Geochemistry","score_opus":0.021527838382841384,"score_gpt":0.29401674829604485,"score_spread":0.27248890991320346,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2905132918","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99775714,0.0001804094,0.000026095997,0.000027792557,0.0000016613454,0.0000038933367,0.000066748624,0.0000041164126,0.0019321329],"genre_scores_gemma":[0.9993668,0.00008671129,0.00004456845,0.000008097622,0.000002188802,0.0000019929269,0.00020486144,0.0000012430759,0.0002835085],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984634,0.00002071094,0.0000071144186,0.00003583868,0.000022495282,0.000067350855],"domain_scores_gemma":[0.9998795,0.000012644462,0.00004933879,0.0000075678063,0.000027334552,0.000023663755],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015296892,0.0001338696,0.00014267136,0.0014830098,0.00087395206,0.0006724496,0.00034444247,0.00015829955,0.0018141977],"category_scores_gemma":[0.0002993468,0.000055138524,0.00011823932,0.0017746802,0.0005859332,0.00018380245,0.0006044106,0.00023069626,0.000115749244],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020070025,0.000035515743,0.9732713,0.00004484266,0.000048638478,0.0008112322,0.00373437,0.00030108684,0.004812471,0.00063982623,0.00019362048,0.01590634],"study_design_scores_gemma":[0.0000031323807,0.000010449946,0.9979482,0.000008672683,0.0000056910108,0.0000927069,0.0012116181,0.00010015921,0.000100085876,0.000043257845,0.000473788,0.0000022164336],"about_ca_topic_score_codex":0.26545137,"about_ca_topic_score_gemma":0.46276993,"teacher_disagreement_score":0.7345486,"about_ca_system_score_codex":0.0013698968,"about_ca_system_score_gemma":0.0007399882,"threshold_uncertainty_score":0.52781254},"labels":[],"label_agreement":null},{"id":"W2906161517","doi":"10.1029/2018jb016226","title":"Quartz Flow Law Revisited: The Significance of Pressure Dependence of the Activation Enthalpy","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Northwest University; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Mylonite; Creep; Dislocation creep; Strain rate; Geology; Quartz; Rheology; Mechanics; Thermodynamics; Law; Materials science; Shear zone; Physics","score_opus":0.040913919148463436,"score_gpt":0.3160859965273456,"score_spread":0.27517207737888216,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2906161517","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95654273,0.0013269574,0.034693997,0.00072485907,0.000075122145,0.00007836104,0.0004097534,0.0003555639,0.005792638],"genre_scores_gemma":[0.9985115,0.00012968498,0.0010711058,0.00003106111,0.000015306534,0.0000130497665,0.000042501164,0.000013529783,0.00017217439],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99959093,0.000056923902,0.000027480359,0.000179433,0.00010784481,0.000037304915],"domain_scores_gemma":[0.99841475,0.0009625776,0.00027214107,0.00015112171,0.0001668901,0.000032431028],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011863721,0.00027924898,0.00032566924,0.0008658176,0.0002218003,0.0005721857,0.00075198826,0.00042959466,0.0016185782],"category_scores_gemma":[0.0037258305,0.00019584622,0.00023530201,0.0003067919,0.0013673707,0.001204416,0.00037126648,0.00077219453,0.00016969918],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047516145,0.00039362075,0.09179732,0.0006301849,0.000105724896,0.00087805087,0.00060486846,0.123632714,0.67494184,0.041896116,0.0018085449,0.06283584],"study_design_scores_gemma":[0.00007384982,0.00082813436,0.15614101,0.000088593246,0.000047043755,0.0004329006,0.000181238,0.542364,0.26826996,0.027153494,0.0043172645,0.00010255046],"about_ca_topic_score_codex":0.0015564797,"about_ca_topic_score_gemma":0.0009425792,"teacher_disagreement_score":0.0016185782,"about_ca_system_score_codex":0.00048110733,"about_ca_system_score_gemma":0.0002750918,"threshold_uncertainty_score":0.0062742233},"labels":[],"label_agreement":null},{"id":"W2906472891","doi":"10.1029/2018jb016828","title":"Extent of Low‐Angle Normal Slip in the 2010 El Mayor‐Cucapah (Mexico) Earthquake From Differential Lidar","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"U.S. Geological Survey","keywords":"Geology; Slip (aerodynamics); Seismology; Geodetic datum; Geodesy; Fault (geology); Magnetic dip; Fault trace; Fault plane; Surface rupture; Earthquake rupture; Strike-slip tectonics; Geometry; Physics; Geophysics","score_opus":0.03790430668542853,"score_gpt":0.3107501089246101,"score_spread":0.27284580223918153,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2906472891","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99930537,0.000016702868,0.000039674356,0.000015025723,8.346346e-7,0.0000020011228,0.0002689764,0.0000056749354,0.0003456841],"genre_scores_gemma":[0.99944943,0.0000151449885,0.00009194835,0.000004342581,0.000001984161,0.0000033781698,0.00034421662,9.870132e-7,0.0000885685],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999385,0.00000554756,0.0000031951702,0.000019158337,0.000013753328,0.000019862047],"domain_scores_gemma":[0.99983454,0.000022063963,0.000060325532,0.000012380917,0.000049370552,0.000021329075],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001321575,0.00013190645,0.00013243717,0.00075530156,0.00028800915,0.0003508098,0.0002601604,0.00031926844,0.00058297144],"category_scores_gemma":[0.00038396727,0.00012219009,0.00007939716,0.0007639134,0.00019248133,0.00023628694,0.00036737934,0.00018002611,0.00010587023],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011101682,0.000068101544,0.9813286,0.000022756101,0.000026496105,0.0002364813,0.00033948896,0.0021624956,0.006159449,0.000062400475,0.00035262556,0.009130131],"study_design_scores_gemma":[0.0000039084293,0.000012065544,0.9970457,0.0000036204265,0.0000041153844,0.000030563217,0.00021432363,0.0022966505,0.0002053175,0.000009130362,0.00017138929,0.0000031845113],"about_ca_topic_score_codex":0.060461838,"about_ca_topic_score_gemma":0.09582712,"teacher_disagreement_score":0.060461838,"about_ca_system_score_codex":0.0005265335,"about_ca_system_score_gemma":0.00023625742,"threshold_uncertainty_score":0.12021983},"labels":[],"label_agreement":null},{"id":"W2906967575","doi":"10.1029/2018jb016681","title":"GIGJ: A Crustal Gravity Model of the Guangdong Province for Predicting the Geoneutrino Signal at the JUNO Experiment","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Snolab","funders":"Nuclear Physics; Università degli Studi di Ferrara","keywords":"Inversion (geology); Crust; Bouguer anomaly; A priori and a posteriori; Depth sounding; Gravitational field; Standard deviation","score_opus":0.06116841028867718,"score_gpt":0.31171802983050595,"score_spread":0.25054961954182875,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2906967575","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9630317,0.00016431723,0.029789006,0.00027342924,0.000030339828,0.000041766307,0.0020926744,0.0005983076,0.0039786343],"genre_scores_gemma":[0.9926448,0.000053112777,0.005341884,0.000016610888,0.0000074911845,0.000022031636,0.0010749719,0.000034904435,0.0008043393],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999397,0.000010874045,0.000002965736,0.000022921553,0.00001047046,0.0000129987],"domain_scores_gemma":[0.9998872,0.000028637243,0.000017853436,0.000013297884,0.000029041592,0.000023842533],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024561104,0.0006606288,0.0003135423,0.0003792497,0.0003986839,0.00064613245,0.000978682,0.0006704521,0.0012635322],"category_scores_gemma":[0.00055741926,0.00035500058,0.0005044107,0.000427736,0.00037881447,0.00031623215,0.00050169934,0.00043409513,0.00017281626],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000031553715,0.000016222028,0.008891568,0.000008950507,0.000017822462,0.000041928244,0.000015207259,0.9875187,0.00082407834,0.00040692606,0.00025223327,0.0019748074],"study_design_scores_gemma":[0.000008779805,0.0000031162797,0.0017722051,7.9515354e-7,0.0000028582033,0.0000019457489,0.0000031301715,0.99799037,0.000060105835,0.00006831674,0.00008550929,0.0000029359876],"about_ca_topic_score_codex":0.23550282,"about_ca_topic_score_gemma":0.10057986,"teacher_disagreement_score":0.23550282,"about_ca_system_score_codex":0.0012061537,"about_ca_system_score_gemma":0.001863252,"threshold_uncertainty_score":0.4682641},"labels":[],"label_agreement":null},{"id":"W2908797411","doi":"10.1029/2018jb016627","title":"<i>P</i> Wave Teleseismic Traveltime Tomography of the North American Midcontinent","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal; University of Manitoba","funders":"National Science Foundation","keywords":"Geology; Seismology; Rift; Terrane; Mantle (geology); Subduction; Crust; Lithosphere; Bouguer anomaly; Geophysics; Tectonics; Paleontology; Gravity anomaly","score_opus":0.017837295537918567,"score_gpt":0.26188113630407267,"score_spread":0.2440438407661541,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2908797411","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977501,0.000054585387,0.00028852656,0.000055556557,0.0000029587031,0.000003240522,0.00063115865,0.00004140276,0.0011724842],"genre_scores_gemma":[0.99825877,0.000055361525,0.0008095123,0.000015818623,0.0000052115597,0.0000036391261,0.0004956554,0.000006057051,0.00034985805],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999776,0.0000024904357,0.0000011674754,0.000007703279,0.0000057445036,0.000005292615],"domain_scores_gemma":[0.999876,0.000011901634,0.000027181813,0.0000101499745,0.00005329387,0.00002149791],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000092433205,0.00015174148,0.000071072245,0.00080189557,0.00021946381,0.0003119736,0.00018473718,0.00012522057,0.0009282531],"category_scores_gemma":[0.0002541627,0.0000884979,0.00007457202,0.00070114597,0.00009041048,0.00015093165,0.00017873358,0.000117292984,0.0001529673],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000864883,0.000058000416,0.92984366,0.00002883772,0.000055988432,0.0003848548,0.0005949951,0.005087341,0.026791845,0.00033977668,0.0020137506,0.03471434],"study_design_scores_gemma":[0.000005032094,0.0000104424935,0.9920574,0.000007719752,0.0000131776815,0.000054411128,0.00019675336,0.0056403424,0.0005972643,0.000057245878,0.0013557228,0.0000045123234],"about_ca_topic_score_codex":0.07236472,"about_ca_topic_score_gemma":0.17200728,"teacher_disagreement_score":0.07236472,"about_ca_system_score_codex":0.00038430252,"about_ca_system_score_gemma":0.0004071879,"threshold_uncertainty_score":0.14388704},"labels":[],"label_agreement":null},{"id":"W2910387435","doi":"10.1029/2018jb016482","title":"Extrinsic Elastic Anisotropy in a Compositionally Heterogeneous Earth's Mantle","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"H2020 European Research Council; Natural Environment Research Council; Sight Research UK","keywords":"Anisotropy; Geology; Layering; Seismic anisotropy; Mantle (geology); Isotropy; Geophysics; Basalt; Crust; Mineralogy; Seismology; Optics; Physics","score_opus":0.02331398454708357,"score_gpt":0.2945363944568419,"score_spread":0.2712224099097583,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2910387435","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9941474,0.00006740273,0.0046920795,0.000018050769,0.0000013014563,0.0000034807224,0.00010582258,0.000043889082,0.00092046283],"genre_scores_gemma":[0.9994838,0.0000276063,0.00035083585,0.0000023464122,0.0000013764226,0.0000012270209,0.000066097185,0.0000052985038,0.00006135722],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999188,0.000011085979,0.0000049913556,0.000027252983,0.000021797188,0.000015986998],"domain_scores_gemma":[0.9998024,0.00007121495,0.000048449743,0.00002493986,0.000037916812,0.000015022204],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026335203,0.00035724606,0.00017828796,0.00088869024,0.00013461293,0.00044996565,0.00033462135,0.00020296141,0.0005935545],"category_scores_gemma":[0.00078477664,0.00026898427,0.00020737867,0.0004962514,0.00038410054,0.00048796434,0.00042216445,0.00017855744,0.000077920275],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033489277,0.000051685587,0.10097358,0.00012381618,0.00020876662,0.00056917197,0.00013838524,0.17938614,0.7006025,0.0075138505,0.00012142924,0.0099757165],"study_design_scores_gemma":[0.00005023065,0.00008084145,0.3751132,0.000015011104,0.00010967491,0.00028985797,0.00010731959,0.55435294,0.06472067,0.004334966,0.00077350246,0.00005176695],"about_ca_topic_score_codex":0.0020931698,"about_ca_topic_score_gemma":0.0014445473,"teacher_disagreement_score":0.0020931698,"about_ca_system_score_codex":0.0003062171,"about_ca_system_score_gemma":0.0001049309,"threshold_uncertainty_score":0.0041620135},"labels":[],"label_agreement":null},{"id":"W2910628911","doi":"10.1029/2018jb016505","title":"Magnetotelluric Evidence for Asymmetric Simple Shear Extension and Lithospheric Thinning in South China","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":72,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"National Key Research and Development Program of China; U.S. Geological Survey; National Natural Science Foundation of China; Compute Canada","keywords":"Geology; Lithosphere; Rift; Mantle (geology); Shear zone; Seismology; Petrology; Geophysics; Paleontology; Tectonics","score_opus":0.06927030624037428,"score_gpt":0.36535075256123584,"score_spread":0.29608044632086156,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2910628911","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995566,0.00004048383,0.00005916017,0.000011513533,6.9396623e-7,0.0000012580973,0.0001444383,0.000005740963,0.00018007774],"genre_scores_gemma":[0.9996099,0.00002416268,0.000071539514,0.0000059160643,0.0000017778465,0.00000228551,0.0002143699,0.0000013560971,0.00006873421],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999037,0.0000084316625,0.000008864598,0.000038233124,0.000023393404,0.00001752055],"domain_scores_gemma":[0.9996643,0.000031203388,0.00013577718,0.000037930415,0.00007391827,0.00005692862],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022354742,0.00030148344,0.0002964779,0.0013912355,0.0003771015,0.000298882,0.00025860954,0.00025009827,0.0005895006],"category_scores_gemma":[0.00031251422,0.00023373813,0.00019527471,0.0012867532,0.00044404503,0.00020615911,0.00041486468,0.000116028605,0.00008960788],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006479854,0.0000119398865,0.92781156,0.000041742755,0.00007054857,0.00022572247,0.0005138735,0.00044760914,0.06690872,0.00010207152,0.00008569714,0.0037156884],"study_design_scores_gemma":[0.0000026312193,0.0000072024045,0.9988881,0.0000014128889,0.000007734263,0.00002499395,0.000064476386,0.00025074897,0.00064898754,0.000017976972,0.000083749714,0.0000021634348],"about_ca_topic_score_codex":0.018806864,"about_ca_topic_score_gemma":0.03325796,"teacher_disagreement_score":0.018806864,"about_ca_system_score_codex":0.00046805784,"about_ca_system_score_gemma":0.00036017262,"threshold_uncertainty_score":0.03739482},"labels":[],"label_agreement":null},{"id":"W2912591361","doi":"10.1029/2018jb016556","title":"The Thermal Effects of Plate‐Bending‐Related Thickening of the Oceanic Crustal Aquifer in the Nankai Trough and Japan Trench Subduction Zones","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"National Science Foundation","keywords":"Geology; Aquifer; Subduction; Trench; Oceanic crust; Thickening; Petrology; Crust; Trough (economics); Seismology; Geophysics; Geomorphology; Groundwater; Tectonics; Geotechnical engineering","score_opus":0.01671030225566293,"score_gpt":0.2745217362989993,"score_spread":0.25781143404333634,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2912591361","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99905294,0.000021130098,0.00025314066,0.000020973683,0.0000020930731,0.0000026629848,0.00008290451,0.000015302994,0.00054875476],"genre_scores_gemma":[0.999678,0.000014676812,0.00012138513,0.000005166984,8.84202e-7,0.000002959265,0.000055025583,0.0000046197088,0.00011737951],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999087,0.000020805495,0.000005621737,0.00002560482,0.000008758928,0.000030582712],"domain_scores_gemma":[0.99983394,0.000051012674,0.000034052002,0.000018498204,0.000024426014,0.000037962658],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018008912,0.0005461603,0.00030549016,0.00034836406,0.0004747554,0.0008101847,0.00060163403,0.0005233315,0.0012881659],"category_scores_gemma":[0.00046654776,0.00040309076,0.00077968434,0.00031303783,0.00062527513,0.00044281685,0.00058014784,0.00032455588,0.00007840409],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000093699324,0.000032419623,0.049723573,0.000019319506,0.000077236844,0.000092765025,0.00006405186,0.9420109,0.0064251437,0.00036546102,0.00009201486,0.0010034951],"study_design_scores_gemma":[0.000051732095,0.00007490619,0.058396425,0.000009048177,0.000050538732,0.000030933566,0.00015095217,0.9392342,0.0015203067,0.0002754448,0.00017946643,0.000026085043],"about_ca_topic_score_codex":0.081186205,"about_ca_topic_score_gemma":0.047859065,"teacher_disagreement_score":0.081186205,"about_ca_system_score_codex":0.0018163311,"about_ca_system_score_gemma":0.00067436526,"threshold_uncertainty_score":0.16142732},"labels":[],"label_agreement":null},{"id":"W2913215586","doi":"10.1029/2018jb016499","title":"Beyond Receiver Functions: Green's Function Estimation by Transdimensional Inversion and Its Application to OBS Data","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Japan Society for the Promotion of Science","keywords":"Receiver function; Deconvolution; Algorithm; Computer science; Seismometer; Markov chain Monte Carlo; Geology; Applied mathematics; Bayesian probability; Mathematics; Seismology","score_opus":0.037366614612740094,"score_gpt":0.3019409749755807,"score_spread":0.2645743603628406,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2913215586","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.051415626,0.0001570117,0.94754195,0.00011570749,0.000016861974,0.000017734135,0.00007567736,0.00026821974,0.00039115502],"genre_scores_gemma":[0.3812358,0.00038343293,0.6170822,0.00007022555,0.000035159403,0.000068977366,0.00031434154,0.00008216168,0.0007277445],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999665,0.00015708679,0.000022056647,0.000064865075,0.000069306996,0.00002161292],"domain_scores_gemma":[0.9986468,0.00070834334,0.00017282405,0.00018218516,0.00025000153,0.000039839357],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013175017,0.0005347377,0.00028379948,0.0010572729,0.00027532165,0.0006154405,0.00056467444,0.0006590824,0.00056894694],"category_scores_gemma":[0.004633774,0.00025483774,0.000494003,0.0010295729,0.0005457891,0.0008553532,0.0008370943,0.0005986608,0.00017195691],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012652138,0.00010203615,0.017799843,0.00016216782,0.00015663511,0.00026597525,0.00033078008,0.6054075,0.04065188,0.024155973,0.0010319798,0.3098087],"study_design_scores_gemma":[0.000005760121,0.000008084022,0.0013808084,0.0000051349657,0.000006177527,0.00003440813,0.000011976604,0.99398744,0.0019930697,0.0021305836,0.00042390305,0.000012631514],"about_ca_topic_score_codex":0.007013403,"about_ca_topic_score_gemma":0.005660094,"teacher_disagreement_score":0.007013403,"about_ca_system_score_codex":0.00036983812,"about_ca_system_score_gemma":0.0007691592,"threshold_uncertainty_score":0.013945162},"labels":[],"label_agreement":null},{"id":"W2914568489","doi":"10.1029/2018jb016221","title":"The 12 November 2017 <i>M</i><sub><i>w</i></sub> 7.3 Ezgeleh‐Sarpolzahab (Iran) Earthquake and Active Tectonics of the Lurestan Arc","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":90,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; National Aeronautics and Space Administration; Canada Research Chairs; Royal Society; Canada Foundation for Innovation; National Science Foundation","keywords":"Geology; Seismology; Aftershock; Basement; Escarpment; Tectonics; Fault (geology); Thrust fault; Induced seismicity; Geomorphology","score_opus":0.02879129617149324,"score_gpt":0.2812676163740509,"score_spread":0.25247632020255767,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2914568489","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99028766,0.00024535484,0.0002391944,0.00026148712,0.00005826176,0.000019444244,0.0015116781,0.000042778007,0.0073342077],"genre_scores_gemma":[0.9932106,0.00022402886,0.0002106006,0.00004629212,0.00009273662,0.0000070982455,0.0032582534,0.000011440796,0.0029389795],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999244,0.00000416051,0.000003155628,0.000012732775,0.00002644832,0.000029083363],"domain_scores_gemma":[0.99987245,0.0000036975537,0.000056352823,0.000009445763,0.000034804958,0.000023161077],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009225067,0.00018113153,0.00017996055,0.0006512136,0.00026220983,0.0003615144,0.00014090579,0.00017955535,0.0019379457],"category_scores_gemma":[0.00015775845,0.000063401516,0.0001457701,0.0006383367,0.0002861139,0.00015612908,0.00042789325,0.00020446829,0.00053771754],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000330306,0.00013737043,0.8855274,0.0001305217,0.000130722,0.0018506467,0.00064020196,0.0013955213,0.017631916,0.00080841326,0.018645747,0.07277117],"study_design_scores_gemma":[0.0000051271436,0.000019634022,0.99504447,0.000007784979,0.000007917732,0.00014844991,0.00017279845,0.00028314858,0.0005169279,0.000046933535,0.0037439545,0.0000027864817],"about_ca_topic_score_codex":0.010305854,"about_ca_topic_score_gemma":0.02239515,"teacher_disagreement_score":0.010305854,"about_ca_system_score_codex":0.0004211058,"about_ca_system_score_gemma":0.00046646732,"threshold_uncertainty_score":0.02049172},"labels":[],"label_agreement":null},{"id":"W2916883523","doi":"10.1029/2018jb016485","title":"Magma Reservoir Below Laguna del Maule Volcanic Field, Chile, Imaged With Surface‐Wave Tomography","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University; University of Alberta","funders":"National Science Foundation","keywords":"Geology; Magma; Volcano; Seismology; Magma chamber; Crust; Magnetotellurics; Caldera; Seismic tomography; Geophysics; Rhyolite; Petrology; Volcanic rock; Mantle (geology)","score_opus":0.019787673622479816,"score_gpt":0.2717555057904545,"score_spread":0.2519678321679747,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2916883523","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9939168,0.00013304806,0.0016048185,0.00009996383,0.0000035828475,0.000027915901,0.0011484132,0.0001484996,0.0029169836],"genre_scores_gemma":[0.9978611,0.00007654587,0.0011055984,0.000011255855,0.0000031395955,0.000018030463,0.0004232458,0.000010989662,0.0004902644],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996495,0.0000024736148,0.0000025100803,0.000009770358,0.000010711335,0.00000956909],"domain_scores_gemma":[0.99987316,0.000023795496,0.000033692282,0.000014975004,0.000035002904,0.000019273617],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000105269944,0.00028080202,0.00015583161,0.0012280904,0.00020805086,0.00069889915,0.0003873598,0.000360192,0.0010466988],"category_scores_gemma":[0.0005016343,0.00026546407,0.00015853143,0.0009589786,0.00024171606,0.00049441116,0.0003718536,0.00021112469,0.00022919137],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029315628,0.00017080992,0.80527705,0.00017448408,0.00013101022,0.0020026164,0.0015537721,0.040631074,0.10182286,0.0011793242,0.0018868019,0.044877045],"study_design_scores_gemma":[0.00004854435,0.000047377056,0.8951045,0.000041893843,0.000035190216,0.0003468423,0.0006752676,0.098022245,0.0035127783,0.00041694773,0.0017185806,0.00002984761],"about_ca_topic_score_codex":0.04731713,"about_ca_topic_score_gemma":0.045391772,"teacher_disagreement_score":0.04731713,"about_ca_system_score_codex":0.00073026115,"about_ca_system_score_gemma":0.0008180517,"threshold_uncertainty_score":0.09408343},"labels":[],"label_agreement":null},{"id":"W2917203534","doi":"10.1029/2018jb016352","title":"Shear Wave Splitting Discloses Two Episodes of Collision‐Related Convergence in Western North America","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Australian Research Council; Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Seismic anisotropy; Shear wave splitting; Lithosphere; Anisotropy; Seismology; Crust; Mantle (geology); Foothills; Shear (geology); Geophysics; Tectonics; Petrology","score_opus":0.02845841047324545,"score_gpt":0.30994770144395184,"score_spread":0.2814892909707064,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2917203534","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99970776,0.000023209375,0.000017150773,0.000004228737,3.3319688e-7,0.0000015704345,0.00007064974,0.0000012839449,0.00017375353],"genre_scores_gemma":[0.999559,0.000030811825,0.0000640419,0.0000035188864,8.772057e-7,0.0000033220394,0.00025773022,0.0000010469703,0.000079660844],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998721,0.000013685428,0.000009307125,0.000031528172,0.00003177518,0.000041614494],"domain_scores_gemma":[0.9996724,0.00004359987,0.000095311545,0.000025668221,0.00009796676,0.00006504073],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018458172,0.00013372798,0.00015982184,0.0011282449,0.0005768998,0.00043036364,0.00017300107,0.0002006415,0.00043453043],"category_scores_gemma":[0.0005380456,0.00020187943,0.00009027256,0.0012974575,0.00040129563,0.00017084248,0.0004322518,0.00011688902,0.00005139686],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006786874,0.0000122514875,0.9891643,0.000010299092,0.000033813638,0.00017312358,0.0014245098,0.00014840574,0.0044913343,0.000049617767,0.00012075397,0.0043037212],"study_design_scores_gemma":[7.070446e-7,0.00000253787,0.99942833,0.0000012523269,0.0000034137615,0.000019977908,0.00028995244,0.000081046455,0.00006013546,0.000005075568,0.0001064517,0.0000011187353],"about_ca_topic_score_codex":0.31263003,"about_ca_topic_score_gemma":0.6174347,"teacher_disagreement_score":0.31263003,"about_ca_system_score_codex":0.0011560038,"about_ca_system_score_gemma":0.00087160815,"threshold_uncertainty_score":0.62162066},"labels":[],"label_agreement":null},{"id":"W2918933619","doi":"10.1029/2018jb016242","title":"Lithospheric Signature of Late Cenozoic Extension in Electrical Resistivity Structure of the Rio Grande Rift, New Mexico, USA","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"University of Colorado Boulder; U.S. Bureau of Land Management; U.S. Geological Survey; Geological Society of America; U.S. Forest Service; University of Alberta; National Science Foundation","keywords":"Geology; Lithosphere; Rift; Magnetotellurics; Crust; Mantle (geology); Geophysics; Seismology; Electrical resistivity and conductivity; Petrology; Tectonics","score_opus":0.021916441970353785,"score_gpt":0.3019831614532851,"score_spread":0.28006671948293127,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2918933619","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998376,0.000033123204,0.00011434793,0.00007502461,0.0000012016931,0.0000019371691,0.00038769512,0.000021120655,0.0009896592],"genre_scores_gemma":[0.99935955,0.000025753547,0.00010946191,0.0000056380964,0.0000018554933,0.0000027310869,0.00034787453,0.0000026705068,0.0001443568],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999732,0.000003859784,0.0000011753348,0.000010344046,0.000004723409,0.000006669847],"domain_scores_gemma":[0.99989057,0.000020664664,0.00003971202,0.000009626142,0.000028538565,0.000010897086],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007368024,0.00013339902,0.000080844504,0.0003495647,0.00016463193,0.00032617289,0.00017932268,0.00017760029,0.0006727441],"category_scores_gemma":[0.0003361262,0.000090644426,0.00011920781,0.00032467442,0.00014526004,0.00014119374,0.0002270977,0.00010447622,0.00006917762],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001109366,0.000038370996,0.9660482,0.000023683937,0.000072748444,0.0002126951,0.00033890913,0.015671447,0.0092159975,0.00027265595,0.0007222315,0.0072721713],"study_design_scores_gemma":[0.000010538807,0.000010963267,0.99052495,0.0000056555555,0.000010382932,0.000024656087,0.00012979067,0.008407661,0.00024620924,0.000035876925,0.00058866694,0.0000047414055],"about_ca_topic_score_codex":0.09408243,"about_ca_topic_score_gemma":0.14192837,"teacher_disagreement_score":0.09408243,"about_ca_system_score_codex":0.00044351007,"about_ca_system_score_gemma":0.00022050289,"threshold_uncertainty_score":0.1870696},"labels":[],"label_agreement":null},{"id":"W2922383903","doi":"10.1029/2018jb016894","title":"Along‐Strike Variations in Structure of the Continent‐Ocean Transition at the Northeastern Nova Scotia Margin From Wide‐Angle Seismic Observations","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"Offshore Energy Research Association","keywords":"Geology; Crust; Oceanic crust; Mantle (geology); Transition zone; Continental crust; Continental margin; Nova scotia; Seismology; Petrology; Geophysics; Subduction; Tectonics; Oceanography","score_opus":0.03158199170843658,"score_gpt":0.2691691222688853,"score_spread":0.23758713056044872,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2922383903","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967289,0.00006314788,0.000115684314,0.000026622492,0.0000034158977,0.000006621158,0.0011055305,0.000015140076,0.001934856],"genre_scores_gemma":[0.99890494,0.000038026836,0.00007584076,0.000007271391,7.0265435e-7,0.0000023503953,0.0005270429,0.0000030690564,0.0004406809],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999453,0.000004708728,0.0000034799907,0.000016235455,0.000012547295,0.00001778895],"domain_scores_gemma":[0.99978286,0.00001899777,0.00004324237,0.00001444351,0.00008884096,0.000051647203],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011375613,0.0002112002,0.00009576293,0.0005723971,0.00033224962,0.000700403,0.00018525313,0.00015795186,0.0014163535],"category_scores_gemma":[0.0004595111,0.00015935831,0.00019074624,0.00045754178,0.00021326198,0.00011472379,0.0003279721,0.00010874209,0.00024457395],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008438862,0.000012585991,0.97803885,0.0000229968,0.000060664188,0.00017965568,0.00024922675,0.009791881,0.0058421637,0.00017681303,0.0006131571,0.0049276077],"study_design_scores_gemma":[0.0000042810066,0.0000045275688,0.99603975,0.000008536245,0.000005696026,0.000016703612,0.000103105085,0.0033445498,0.00011462934,0.000015461685,0.00033969383,0.0000031529069],"about_ca_topic_score_codex":0.8311496,"about_ca_topic_score_gemma":0.88658524,"teacher_disagreement_score":0.16885042,"about_ca_system_score_codex":0.0021802462,"about_ca_system_score_gemma":0.0016290147,"threshold_uncertainty_score":0.3396896},"labels":[],"label_agreement":null},{"id":"W2923321653","doi":"10.1029/2018jb017150","title":"Delayed Dynamic Triggering of Disposal‐Induced Earthquakes Observed by a Dense Array in Northern Oklahoma","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Seismology; Induced seismicity; Geology; Fault (geology); Slip (aerodynamics)","score_opus":0.036051078539376086,"score_gpt":0.2992183321221412,"score_spread":0.26316725358276516,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2923321653","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99936515,0.000014591578,0.000020643585,0.000023638888,7.5846623e-7,0.0000034398265,0.00022582764,0.0000037096258,0.0003422368],"genre_scores_gemma":[0.9996082,0.000016969909,0.000036096975,0.000008697786,0.0000018637363,0.0000061685364,0.00018448624,8.050964e-7,0.00013673228],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990773,0.000009196986,0.000007195531,0.000022956741,0.000012910692,0.000040101542],"domain_scores_gemma":[0.9994943,0.00006634955,0.00018975008,0.000038185735,0.00007642492,0.00013490026],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011876486,0.00014424171,0.00019028211,0.0008874688,0.000856599,0.00053434103,0.0002855533,0.00028497755,0.0014294813],"category_scores_gemma":[0.00044122394,0.00015478727,0.000097967684,0.0010311415,0.0003235688,0.00030129208,0.00078495726,0.0002320397,0.00013629251],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014037674,0.000091469985,0.98396033,0.000029246603,0.000044912522,0.00047630531,0.0012475987,0.0005677886,0.006901916,0.0000527989,0.00036167348,0.0061256383],"study_design_scores_gemma":[0.000003064077,0.000011391193,0.99847096,0.0000043873924,0.000006713943,0.0000320731,0.0008155528,0.00025339666,0.00017992075,0.0000062246313,0.00021322619,0.0000030587778],"about_ca_topic_score_codex":0.16206475,"about_ca_topic_score_gemma":0.32148325,"teacher_disagreement_score":0.16206475,"about_ca_system_score_codex":0.0013947284,"about_ca_system_score_gemma":0.00083542377,"threshold_uncertainty_score":0.3222428},"labels":[],"label_agreement":null},{"id":"W2928614424","doi":"10.1029/2018jb017050","title":"Seismicity‐Scanning Based on Navigated Automatic Phase‐Picking","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismology and Earthquake Studies","field":"Computer Science","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary; University of Victoria; Geological Survey of Canada","funders":"","keywords":"Induced seismicity; Intersection (aeronautics); Workflow; Set (abstract data type); Computer science; Geology; Seismology; Relation (database); Pattern recognition (psychology); Data mining; Algorithm; Artificial intelligence; Engineering; Database","score_opus":0.041502567876705865,"score_gpt":0.37463867746891166,"score_spread":0.3331361095922058,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2928614424","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.06407571,0.000104514904,0.9298978,0.000045056884,0.000033514036,0.00007194647,0.00028243498,0.0035630763,0.0019259208],"genre_scores_gemma":[0.3294196,0.00006613424,0.66820145,0.000043361426,0.000022984936,0.00009832457,0.0008308817,0.0001929756,0.0011242633],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9995958,0.00007078561,0.000022294891,0.00010359395,0.00016840153,0.000039134124],"domain_scores_gemma":[0.9993204,0.00018828573,0.000093831884,0.00014492788,0.00020083302,0.000051710427],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038786844,0.0005161274,0.00049765775,0.0021852392,0.00030351462,0.00054444023,0.0009537752,0.00039766968,0.0019498235],"category_scores_gemma":[0.0015837785,0.0003443586,0.00043348392,0.0012454678,0.00037044063,0.0007042922,0.0011253881,0.0003469356,0.0010502953],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047147257,0.000107823726,0.011971083,0.00016326531,0.00010813162,0.0003236307,0.0002698595,0.036723427,0.18038382,0.0039432305,0.0034929058,0.7620414],"study_design_scores_gemma":[0.00009859102,0.0002573347,0.013724471,0.000025552978,0.000060685335,0.0013048945,0.0001451889,0.85131943,0.116332315,0.005450839,0.011163595,0.0001171615],"about_ca_topic_score_codex":0.0012324919,"about_ca_topic_score_gemma":0.0025320903,"teacher_disagreement_score":0.0021852392,"about_ca_system_score_codex":0.00019601305,"about_ca_system_score_gemma":0.00074381306,"threshold_uncertainty_score":0.0065227747},"labels":[],"label_agreement":null},{"id":"W2928694646","doi":"10.1029/2018jb016728","title":"Weak B‐Type Olivine Fabric Induced by Fast Compaction of Crystal Mush in a Crustal Magma Reservoir","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"National Natural Science Foundation of China","keywords":"Geology; Olivine; Peridotite; Ultramafic rock; Dislocation creep; Seismic anisotropy; Mafic; Petrology; Mineralogy; Geochemistry; Mantle (geology); Dislocation; Composite material; Materials science","score_opus":0.03163926346265882,"score_gpt":0.30938823547420385,"score_spread":0.277748972011545,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2928694646","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99986994,0.000006045031,0.000037857946,0.0000015844236,1.593615e-7,6.735271e-7,0.000013641109,0.0000040106697,0.000066120636],"genre_scores_gemma":[0.9999082,0.0000036232316,0.000043476477,5.356876e-7,1.5590555e-7,4.9295244e-7,0.00001694511,7.3757707e-7,0.000025886946],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99996185,0.0000019595502,0.0000027277258,0.000011638691,0.0000081721855,0.000013585095],"domain_scores_gemma":[0.99994075,0.000008973788,0.000015469306,0.0000066327902,0.000009743816,0.000018401925],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000055653953,0.0001321135,0.00020064037,0.00036051476,0.00030778034,0.00028629697,0.00024550498,0.00017705467,0.0005003807],"category_scores_gemma":[0.0001671375,0.00016996573,0.000116355004,0.00026193098,0.00031785556,0.00017386446,0.00028418502,0.00012191251,0.00005449898],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005156302,0.000082057944,0.22903886,0.000077898934,0.00006644121,0.0019341588,0.00024666535,0.011487706,0.75178206,0.00024408915,0.00006125096,0.0044632154],"study_design_scores_gemma":[0.000035159526,0.00026252118,0.8900755,0.0000064431842,0.000028248456,0.00044251108,0.00030669302,0.038338076,0.07004666,0.00010067692,0.00034167158,0.000015832655],"about_ca_topic_score_codex":0.00592384,"about_ca_topic_score_gemma":0.0056621977,"teacher_disagreement_score":0.00592384,"about_ca_system_score_codex":0.00032711835,"about_ca_system_score_gemma":0.00017013095,"threshold_uncertainty_score":0.011778712},"labels":[],"label_agreement":null},{"id":"W2937230386","doi":"10.1029/2018jb016673","title":"A Diagenesis Model for Geomechanical Simulations: Formulation and Implications for Pore Pressure and Development of Geological Structures","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Hydraulic Fracturing and Reservoir Analysis","field":"Engineering","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"Engineering and Physical Sciences Research Council; Natural Environment Research Council; Sight Research UK","keywords":"Diagenesis; Geology; Overpressure; Pore water pressure; Cementation (geology); Pressure solution; Porosity; Geotechnical engineering; Effective stress; Compaction; Permeability (electromagnetism); Brittleness; Petrology; Mineralogy; Materials science; Cement; Thermodynamics","score_opus":0.04660706122527573,"score_gpt":0.34018396988192323,"score_spread":0.2935769086566475,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2937230386","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.40752417,0.00035478125,0.5628342,0.0009597501,0.00012640275,0.00032055486,0.00090682926,0.00091161916,0.026061585],"genre_scores_gemma":[0.95558536,0.00021530112,0.038275827,0.00009654534,0.00003287419,0.00035217352,0.0002434048,0.00013656936,0.005061963],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998952,0.00003667312,0.000007596407,0.000018775327,0.000027423184,0.0000142641575],"domain_scores_gemma":[0.99971145,0.00014221083,0.000037736532,0.000020604353,0.00005719906,0.00003068064],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033937927,0.00058104267,0.0004841,0.00033147354,0.00046558862,0.0010053086,0.001014495,0.0017389355,0.002079654],"category_scores_gemma":[0.00075694476,0.00042109314,0.0004847925,0.00029917134,0.00080912263,0.0005536244,0.0007320024,0.0009001147,0.00022387909],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000070847823,0.000019897561,0.00039923855,0.000009467656,0.0000044991934,0.000038355713,0.000011902618,0.99439174,0.001252509,0.0030448802,0.000073738855,0.0007467374],"study_design_scores_gemma":[0.0000030328526,0.000004677147,0.000057862202,0.000001273456,9.778051e-7,0.0000026838802,0.0000025861307,0.9993481,0.0001594844,0.0002936278,0.00012416014,0.0000014174856],"about_ca_topic_score_codex":0.009806784,"about_ca_topic_score_gemma":0.006350119,"teacher_disagreement_score":0.009806784,"about_ca_system_score_codex":0.0009984057,"about_ca_system_score_gemma":0.0010493885,"threshold_uncertainty_score":0.019499421},"labels":[],"label_agreement":null},{"id":"W2937651902","doi":"10.1029/2018jb017039","title":"Induced Seismicity Driven by Fluid Diffusion Revealed by a Near‐Field Hydraulic Stimulation Monitoring Array in the Montney Basin, British Columbia","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Research School, Ruhr University Bochum","keywords":"Induced seismicity; Geology; Hydraulic fracturing; Seismology; Seismometer; Poromechanics; Geotechnical engineering","score_opus":0.024480550376738904,"score_gpt":0.2877279363336582,"score_spread":0.26324738595691927,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2937651902","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99866056,0.000022499567,0.000087163375,0.000026191365,7.475947e-7,0.000005305198,0.00031145537,0.00001244451,0.0008736719],"genre_scores_gemma":[0.99912506,0.000022130846,0.00012040546,0.000008852696,8.020656e-7,0.0000042739944,0.00020484197,0.0000018028619,0.0005118357],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998603,0.000010132986,0.0000053101635,0.000032479777,0.000050025985,0.00004164767],"domain_scores_gemma":[0.99960095,0.000031619547,0.00006702342,0.00001873189,0.00019226818,0.00008940798],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010254275,0.00014751262,0.0001771423,0.00106869,0.00070154865,0.00051631016,0.0003597015,0.00022223893,0.00078399846],"category_scores_gemma":[0.00042562748,0.00014915843,0.00006354994,0.0013434816,0.00037633642,0.00016034128,0.00049072894,0.00018282747,0.00009995738],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001403898,0.00007410097,0.93909734,0.000030880514,0.00004745833,0.0003961635,0.00133565,0.0021669467,0.033187293,0.00013885483,0.0010606643,0.022324136],"study_design_scores_gemma":[0.0000033304982,0.00001068606,0.9973029,0.000003899239,0.0000049924847,0.000029224168,0.00051426,0.0011529005,0.00042237152,0.000011883975,0.00053729303,0.000006258701],"about_ca_topic_score_codex":0.9017951,"about_ca_topic_score_gemma":0.9676001,"teacher_disagreement_score":0.09820491,"about_ca_system_score_codex":0.0033198723,"about_ca_system_score_gemma":0.0030342282,"threshold_uncertainty_score":0.19756645},"labels":[],"label_agreement":null},{"id":"W2941282361","doi":"10.1029/2018jb016726","title":"Mapping Curie Depth Across Western Canada From a Wavelet Analysis of Magnetic Anomaly Data","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Ocean Networks Canada Society; University of Victoria; University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada; U.S. Geological Survey","keywords":"Craton; Geology; Magnetic anomaly; Curie temperature; Geothermal gradient; Geophysics; Curie; Seismology; Tectonics; Condensed matter physics; Ferromagnetism; Physics","score_opus":0.06623908994715041,"score_gpt":0.3539963593869194,"score_spread":0.287757269439769,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2941282361","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970927,0.00003321504,0.0013146029,0.000035443285,0.0000017171492,0.000007002217,0.000553798,0.00008985946,0.00087161],"genre_scores_gemma":[0.99766845,0.000035416164,0.0014705571,0.0000059274353,7.0291054e-7,0.0000022912266,0.00052063353,0.000008097085,0.0002879856],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999095,0.0000034156137,0.0000024018257,0.000018283832,0.000029855777,0.000036589656],"domain_scores_gemma":[0.9996766,0.000029958876,0.000035374254,0.000013901141,0.0001926232,0.000051625415],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012116083,0.0002674619,0.00013610485,0.0009317611,0.00047777072,0.00053248426,0.00031107874,0.00016228718,0.00051726506],"category_scores_gemma":[0.0006811756,0.000107624975,0.0001609873,0.0009168626,0.00021438082,0.00012940544,0.00025356727,0.00021643713,0.000077268174],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041629426,0.0000824948,0.76166487,0.000081361664,0.00016392804,0.00058726163,0.0010227647,0.080787964,0.046014916,0.0013069477,0.0027352236,0.105136134],"study_design_scores_gemma":[0.00002403253,0.000017053955,0.7614033,0.000020003134,0.000039805687,0.00004788121,0.00074225885,0.22730912,0.007969984,0.00021691537,0.0021801682,0.000029434601],"about_ca_topic_score_codex":0.9387122,"about_ca_topic_score_gemma":0.9646673,"teacher_disagreement_score":0.06128782,"about_ca_system_score_codex":0.003289324,"about_ca_system_score_gemma":0.00470378,"threshold_uncertainty_score":0.12329745},"labels":[],"label_agreement":null},{"id":"W2946789848","doi":"10.1029/2018jb016885","title":"Frictional State Evolution During Normal Stress Perturbations Probed With Ultrasonic Waves","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"National Science Foundation of Sri Lanka; Pennsylvania State University; University of Pennsylvania; National Science Foundation","keywords":"Amplitude; Shearing (physics); Slip (aerodynamics); Mechanics; Shear (geology); Geology; Ultrasonic sensor; Materials science; Stress (linguistics); Shear stress; Seismology; Geotechnical engineering; Composite material; Physics; Optics; Acoustics; Thermodynamics","score_opus":0.017218088273376293,"score_gpt":0.2646196022364902,"score_spread":0.24740151396311394,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2946789848","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994993,0.000014983645,0.00035930652,0.000003550334,7.940927e-7,0.00000147216,0.00001565976,0.0000072688586,0.000097602635],"genre_scores_gemma":[0.9998325,0.000009460063,0.0000868782,0.0000012649591,4.5869652e-7,0.0000013261614,0.000015630181,0.0000011655983,0.00005129447],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999212,0.000009479434,0.0000037468778,0.000014873785,0.000025161504,0.000025574782],"domain_scores_gemma":[0.99988234,0.00003629818,0.00003094998,0.0000135414475,0.000018937451,0.000017902912],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000118285316,0.00013076344,0.00016755702,0.00021385451,0.00010898885,0.00030058943,0.00018043787,0.0001774603,0.00047640482],"category_scores_gemma":[0.00043099525,0.00012080448,0.00008393215,0.00016725836,0.0003207817,0.00021459431,0.0002676818,0.00018541908,0.00007601233],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003556076,0.00008841092,0.019920213,0.000028402588,0.000016841142,0.0001735766,0.00026323082,0.0054437574,0.96847576,0.0001688486,0.000056438123,0.0050088554],"study_design_scores_gemma":[0.00004988359,0.0015134292,0.3193924,0.000012027472,0.000041523457,0.00035619488,0.00096855994,0.1306463,0.5456502,0.00044832597,0.0008687922,0.000052280546],"about_ca_topic_score_codex":0.00092793914,"about_ca_topic_score_gemma":0.0005843883,"teacher_disagreement_score":0.00092793914,"about_ca_system_score_codex":0.00019128917,"about_ca_system_score_gemma":0.00008993454,"threshold_uncertainty_score":0.0018450618},"labels":[],"label_agreement":null},{"id":"W2946928834","doi":"10.1029/2018jb017043","title":"Stable Forearc Stressed by a Weak Megathrust: Mechanical and Geodynamic Implications of Stress Changes Caused by the M = 9 Tohoku‐Oki Earthquake","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Forearc; Geology; Differential stress; Seismology; Wedge (geometry); Subduction; Submarine pipeline; Tectonics; Deformation (meteorology); Geotechnical engineering; Geometry","score_opus":0.02721908828681515,"score_gpt":0.29467757197549105,"score_spread":0.2674584836886759,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2946928834","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999681,0.000012398109,0.00008586367,0.000009628512,9.897609e-7,0.0000013608759,0.000027925822,0.0000035961214,0.00017726823],"genre_scores_gemma":[0.9998766,0.0000105277,0.000033399167,0.0000032157839,6.962717e-7,0.0000010612097,0.000029236226,0.0000010194193,0.000044170396],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995077,0.0000034521543,0.000004687092,0.000011805461,0.000008404299,0.000020803815],"domain_scores_gemma":[0.99987805,0.000012434895,0.000039402446,0.000012249841,0.000022903076,0.000034930614],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001137558,0.00023512081,0.00027250487,0.00046880625,0.00044754302,0.00047105562,0.00035700263,0.0004315328,0.0008465863],"category_scores_gemma":[0.00023046827,0.00028929877,0.00031190252,0.0003741509,0.000487158,0.00025256138,0.0004218529,0.00022930831,0.00011129613],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00072420173,0.000269393,0.77821845,0.00010023234,0.0001751372,0.0037224304,0.0005609518,0.046054494,0.15612641,0.00064218475,0.00027443006,0.013131689],"study_design_scores_gemma":[0.000011303655,0.0001099849,0.96841484,0.000006210725,0.00003931548,0.00018408503,0.0005417207,0.027260423,0.003113381,0.00015320974,0.00014646756,0.000019049005],"about_ca_topic_score_codex":0.0097235795,"about_ca_topic_score_gemma":0.014711264,"teacher_disagreement_score":0.0097235795,"about_ca_system_score_codex":0.0005045088,"about_ca_system_score_gemma":0.00024765046,"threshold_uncertainty_score":0.019333959},"labels":[],"label_agreement":null},{"id":"W2947840537","doi":"10.1029/2019jb017375","title":"Heat Flow in Earth's Core From Invariant Electrical Resistivity of Fe‐Si on the Melting Boundary to 9 GPa: Do Light Elements Matter?","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Foundation for Innovation","keywords":"Electrical resistivity and conductivity; Materials science; Inner core; Thermodynamics; Condensed matter physics; Analytical Chemistry (journal); Chemistry; Composite material; Physics","score_opus":0.021715591868978597,"score_gpt":0.3034123393188777,"score_spread":0.2816967474498991,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2947840537","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984345,0.00006498491,0.0004934451,0.000047791047,0.000002828917,0.0000024032622,0.00010601694,0.000054202457,0.0007937224],"genre_scores_gemma":[0.9997434,0.000015969812,0.000073951545,0.000004630906,0.0000015026669,0.0000010205215,0.000063965694,0.0000065561726,0.0000889878],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99995553,0.0000040652117,0.0000014525265,0.000011277824,0.000013956528,0.000013696755],"domain_scores_gemma":[0.999918,0.000031725922,0.000016162296,0.0000067487013,0.0000182273,0.000009039291],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009147105,0.00016183025,0.0001911845,0.00026346353,0.00017971036,0.00027350333,0.00021964761,0.00021392202,0.001260188],"category_scores_gemma":[0.0002878535,0.00012418473,0.00012939335,0.00018768232,0.0004924381,0.00030994316,0.00020334747,0.000282795,0.000105997104],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042202085,0.000051492985,0.020445764,0.000121236604,0.000027938268,0.00074733637,0.0004310343,0.008139464,0.95905703,0.0022752944,0.00044498636,0.007836487],"study_design_scores_gemma":[0.000055107594,0.0004609842,0.17201585,0.000046499783,0.00003487206,0.0003355224,0.0005493425,0.13141203,0.6901411,0.0026373873,0.0022650992,0.000046212557],"about_ca_topic_score_codex":0.0019932818,"about_ca_topic_score_gemma":0.00085103716,"teacher_disagreement_score":0.0019932818,"about_ca_system_score_codex":0.00025382705,"about_ca_system_score_gemma":0.00010639863,"threshold_uncertainty_score":0.004215777},"labels":[],"label_agreement":null},{"id":"W2949052461","doi":"10.1029/2018jb016494","title":"Micromechanics of High‐Pressure Compaction in Granular Quartz Aggregates","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Rock Mechanics and Modeling","field":"Engineering","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Compaction; Overburden pressure; Micromechanics; Cementation (geology); Hardening (computing); Materials science; Strain hardening exponent; Geotechnical engineering; Porosity; Granular material; Quartz; Anisotropy; Grain size; Pore water pressure; Composite material; Geology; Mineralogy; Cement; Composite number","score_opus":0.020162707740750293,"score_gpt":0.2910917152027258,"score_spread":0.2709290074619755,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2949052461","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993167,0.000020835738,0.00036905718,0.000008815014,8.480627e-7,0.000004019268,0.000041630225,0.000011012202,0.0002272024],"genre_scores_gemma":[0.9998423,0.00000774821,0.00005858707,0.0000019338645,3.5745038e-7,0.0000014072318,0.000012466606,0.0000010143532,0.00007408134],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99988854,0.00000714942,0.0000072693247,0.000018211473,0.00005020548,0.000028626415],"domain_scores_gemma":[0.999788,0.00004994524,0.00006589547,0.000027371176,0.000032285567,0.000036504563],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000123622,0.00009748636,0.000114093986,0.00027398014,0.0002931391,0.00038787656,0.000169258,0.00019912995,0.001010336],"category_scores_gemma":[0.00026873895,0.00021838277,0.00009380697,0.00019490306,0.0006365457,0.000177816,0.00018809168,0.0002145792,0.000094089715],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016596349,0.000027844764,0.0130729955,0.000030938376,0.0000150220985,0.0003548383,0.00020637164,0.0026554524,0.98102057,0.00016294932,0.000055871915,0.0022312969],"study_design_scores_gemma":[0.000029911509,0.00034649103,0.5126863,0.000007895524,0.000020730482,0.0003891218,0.0006423073,0.01877841,0.46595773,0.00020370458,0.00090696325,0.000030419425],"about_ca_topic_score_codex":0.0051451973,"about_ca_topic_score_gemma":0.006178776,"teacher_disagreement_score":0.0051451973,"about_ca_system_score_codex":0.00042219184,"about_ca_system_score_gemma":0.0001775285,"threshold_uncertainty_score":0.010230482},"labels":[],"label_agreement":null},{"id":"W2954278936","doi":"10.1029/2018jb017072","title":"Late Cretaceous Transtension in the Eastern Tibetan Plateau: Evidence From Postcollisional A‐Type Granite and Syenite in the Changdu Area, China","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Chinese Academy of Sciences; National Natural Science Foundation of China","keywords":"Geology; Transtension; Zircon; Intraplate earthquake; Plateau (mathematics); Geochemistry; Cretaceous; Crust; Subduction; Partial melting; Tectonics; Paleontology; Extensional definition","score_opus":0.0469412619355304,"score_gpt":0.2895762970893245,"score_spread":0.2426350351537941,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2954278936","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996474,0.00006929414,0.000019535693,0.000007992705,0.0000010258183,0.000002089387,0.000026561524,0.0000015588178,0.0002245477],"genre_scores_gemma":[0.9996698,0.000052822612,0.000032760447,0.000008323302,0.000003888617,0.000002920127,0.00011623995,0.0000011461037,0.00011213399],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998586,0.000014374767,0.000014996924,0.00003933789,0.000033855995,0.00003873374],"domain_scores_gemma":[0.99943954,0.000061684164,0.0001543195,0.00003113624,0.00018524504,0.00012812023],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037908123,0.00035608796,0.00025123806,0.0027038094,0.0009164342,0.0007612362,0.00048936007,0.00051676657,0.00064334547],"category_scores_gemma":[0.00043310664,0.00026014028,0.00023358996,0.002592208,0.0007310361,0.00030616455,0.0005169597,0.00022027176,0.00011239004],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000065567176,0.000029552593,0.9793773,0.000025344778,0.000039893894,0.00056779635,0.0016407473,0.000060738515,0.0153043615,0.00004466477,0.000027071594,0.0028169006],"study_design_scores_gemma":[0.000003073641,0.00001290806,0.9988852,0.000003565024,0.000007401632,0.00011699261,0.00061856135,0.00007756863,0.00018392185,0.000008855789,0.00008008116,0.0000017170612],"about_ca_topic_score_codex":0.072182514,"about_ca_topic_score_gemma":0.1267955,"teacher_disagreement_score":0.072182514,"about_ca_system_score_codex":0.000785102,"about_ca_system_score_gemma":0.0007062837,"threshold_uncertainty_score":0.1435247},"labels":[],"label_agreement":null},{"id":"W2954527593","doi":"10.1029/2019jb018115","title":"Seismic and Microseismic Signatures of Fluids in Rocks: Bridging the Scale Gap","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"","keywords":"Microseism; Geology; Seismology; Induced seismicity; Suite; Archaeology; Geography","score_opus":0.023937539214572062,"score_gpt":0.2923716165613959,"score_spread":0.2684340773468238,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2954527593","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6838476,0.22201361,0.02391124,0.013236782,0.0030227243,0.00013327018,0.0040499046,0.00025707466,0.049527843],"genre_scores_gemma":[0.8236624,0.1509589,0.012443644,0.0009329165,0.005615751,0.000073194904,0.00129036,0.00015659592,0.0048661698],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9995443,0.00008435945,0.000077011806,0.00006905676,0.00019030852,0.000034965306],"domain_scores_gemma":[0.995073,0.002891383,0.0007116034,0.00021446458,0.0009990113,0.00011042671],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011679718,0.00021473598,0.00035315633,0.0059930193,0.00033141603,0.002086952,0.00036729005,0.00057868904,0.0021670968],"category_scores_gemma":[0.0044030654,0.00014796483,0.00024644777,0.0055843717,0.0009826532,0.0024320937,0.0013593833,0.0004371102,0.00034277234],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036261196,0.000097697746,0.08096909,0.006880612,0.0002849498,0.0012394233,0.0076558525,0.0015688272,0.020923173,0.010613216,0.011622416,0.8577822],"study_design_scores_gemma":[0.000027866025,0.0006435158,0.5292574,0.0068742465,0.00041382472,0.0023214605,0.0336943,0.0026005148,0.013508472,0.020099932,0.39043993,0.00011846771],"about_ca_topic_score_codex":0.0010367547,"about_ca_topic_score_gemma":0.0029033083,"teacher_disagreement_score":0.0059930193,"about_ca_system_score_codex":0.00029076842,"about_ca_system_score_gemma":0.0006397317,"threshold_uncertainty_score":0.007249713},"labels":[],"label_agreement":null},{"id":"W2954644069","doi":"10.1029/2019jb017467","title":"Inherited Cross‐Strike Faults and Oligocene‐Early Miocene Segmentation of the Main Himalayan Thrust, West Nepal","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada; Ontario Council on Graduate Studies, Council of Ontario Universities","keywords":"Geology; Foreland basin; Basement; Seismology; Fault (geology); Paleontology; Tectonics; Subduction; Thrust fault; Metamorphic rock; Décollement; Tectonic phase; Metamorphism","score_opus":0.02283250751952245,"score_gpt":0.29541520331217747,"score_spread":0.27258269579265504,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2954644069","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988438,0.000055559565,0.00008860241,0.000014191874,4.5953087e-7,0.0000023426835,0.00011796233,0.0000052594182,0.0008716922],"genre_scores_gemma":[0.99963176,0.000036718426,0.00007571508,0.0000033654496,5.521506e-7,0.0000017934365,0.00010737622,0.0000018804485,0.00014086823],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999275,0.000008994402,0.0000061291303,0.000028146098,0.000010470542,0.000018718649],"domain_scores_gemma":[0.999905,0.000016540043,0.000034621164,0.000010923412,0.000020746276,0.000012177233],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009509382,0.00017700823,0.00010926639,0.0009945598,0.00038218114,0.0008935218,0.00024187281,0.00021434751,0.0013131265],"category_scores_gemma":[0.00034498147,0.00020653944,0.0001126195,0.0009090542,0.00037467826,0.00028780987,0.00043846213,0.00015432261,0.00023410881],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013513595,0.0000409309,0.9341663,0.00009481046,0.00011418995,0.0013498609,0.0038972993,0.003400992,0.032195076,0.0007560903,0.00017584387,0.02367343],"study_design_scores_gemma":[0.0000027457097,0.000016767814,0.99651814,0.000009548701,0.000015947693,0.00022991489,0.000534219,0.0015026609,0.0006905108,0.00007658966,0.00039826482,0.0000045974007],"about_ca_topic_score_codex":0.026415592,"about_ca_topic_score_gemma":0.048312515,"teacher_disagreement_score":0.026415592,"about_ca_system_score_codex":0.00053908234,"about_ca_system_score_gemma":0.0002944132,"threshold_uncertainty_score":0.052523673},"labels":[],"label_agreement":null},{"id":"W2955664191","doi":"10.1029/2018jb017066","title":"A Massive Slump on the St. Pierre Slope, A New Perspective on the 1929 Grand Banks Submarine Landslide","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Natural Resources Canada; Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Slumping; Geology; Landslide; Submarine landslide; Seafloor spreading; Seismology; Escarpment; Slump; Bathymetry; Geomorphology; Paleontology; Oceanography; Geography; Archaeology","score_opus":0.03900690010603445,"score_gpt":0.30420218758787876,"score_spread":0.2651952874818443,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2955664191","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9752178,0.002607223,0.00029386263,0.0032073506,0.00013166472,0.000016641006,0.00025118748,0.00001696867,0.018257253],"genre_scores_gemma":[0.99391264,0.001586721,0.00025403206,0.0002657416,0.0001373678,0.0000028540217,0.000114710194,0.0000049834816,0.0037209569],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999025,0.000010350044,0.000002684217,0.000014640653,0.00003528382,0.000034458157],"domain_scores_gemma":[0.9998404,0.000021545538,0.000039474868,0.000009142761,0.000042967087,0.000046586458],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011373249,0.00026387835,0.00013603724,0.0011201863,0.0015694286,0.0015320757,0.00034592845,0.00083267834,0.0021128664],"category_scores_gemma":[0.00025949746,0.0001755821,0.00012389543,0.0008540062,0.0018125379,0.00043087528,0.00074211525,0.0007569469,0.00022759735],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037765864,0.000085704065,0.6345282,0.00036622578,0.00010462079,0.14496763,0.064687096,0.0015506968,0.029036246,0.007218239,0.021297086,0.09578057],"study_design_scores_gemma":[0.0000033456122,0.00005986648,0.91753936,0.00014087118,0.000015728952,0.00878353,0.022910507,0.00026537018,0.0005819136,0.0007562613,0.048921064,0.000022214042],"about_ca_topic_score_codex":0.21054222,"about_ca_topic_score_gemma":0.56261075,"teacher_disagreement_score":0.7894578,"about_ca_system_score_codex":0.0026053677,"about_ca_system_score_gemma":0.0012630912,"threshold_uncertainty_score":0.4186334},"labels":[],"label_agreement":null},{"id":"W2961064253","doi":"10.1029/2019jb017831","title":"Effects of Preexisting Structures on the Seismicity of the Charlevoix Seismic Zone","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Seismology; Induced seismicity; Rift; Hypocenter; Tectonics","score_opus":0.027060179018607092,"score_gpt":0.28552469232827726,"score_spread":0.2584645133096702,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2961064253","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99914634,0.00003096137,0.00012619962,0.000020746913,0.0000022141776,0.0000028411034,0.00008167246,0.000016092139,0.00057284854],"genre_scores_gemma":[0.9996946,0.000017451173,0.000043568747,0.000003913633,7.508558e-7,0.0000012437399,0.00010493907,0.000003162895,0.00013053279],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997428,0.000047694433,0.000020685426,0.00005898071,0.00006171159,0.00006800775],"domain_scores_gemma":[0.9990356,0.00035565422,0.00018144792,0.000105668005,0.00012899832,0.00019263082],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037869657,0.00034001563,0.00023974765,0.000516594,0.00044589714,0.0015081378,0.0005541283,0.00042965898,0.0016646548],"category_scores_gemma":[0.0023106963,0.0002815435,0.00024329431,0.00045945347,0.0006773553,0.00034017596,0.0008070809,0.0003033584,0.00013768338],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00057208457,0.00017655415,0.688721,0.00005378849,0.00014356188,0.0005401346,0.00034189655,0.2715038,0.024522137,0.00082598825,0.000395284,0.012203708],"study_design_scores_gemma":[0.000046488793,0.00023348148,0.8457415,0.000016572107,0.00004616446,0.00008960291,0.0002986577,0.14928675,0.003515965,0.00009331367,0.0006114153,0.000020075591],"about_ca_topic_score_codex":0.10555108,"about_ca_topic_score_gemma":0.105581,"teacher_disagreement_score":0.89444894,"about_ca_system_score_codex":0.0024306262,"about_ca_system_score_gemma":0.0008766188,"threshold_uncertainty_score":0.20987338},"labels":[],"label_agreement":null},{"id":"W2961552234","doi":"10.1029/2019jb017587","title":"Heat Flow in the Western Arctic Ocean (Amerasian Basin)","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Ridge; Arctic; Seafloor spreading; Bathymetry; Oceanic crust; Mid-ocean ridge; Structural basin; Oceanography; Sediment; Geophysics; Geomorphology; Paleontology; Tectonics; Subduction","score_opus":0.044543553516716634,"score_gpt":0.30303939004508984,"score_spread":0.2584958365283732,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2961552234","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960453,0.00060730556,0.00013909399,0.00007520558,0.000011493873,0.000003975454,0.0008217396,0.000012069842,0.0022838013],"genre_scores_gemma":[0.99819034,0.00028002035,0.00031760713,0.00001737581,0.0000061840847,0.000004027147,0.0006337064,0.000003121643,0.0005475789],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999509,0.0000062766717,0.0000030106842,0.000012740035,0.000017246739,0.0000097830225],"domain_scores_gemma":[0.9998691,0.000013677271,0.000032591426,0.0000041249054,0.00006288762,0.000017579492],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015257705,0.00014375811,0.000058408896,0.00044578325,0.00026014948,0.00036366636,0.00010346771,0.0000747771,0.00050444796],"category_scores_gemma":[0.00028738542,0.0000696363,0.00012659174,0.00071082753,0.00016204781,0.00017443486,0.00020509861,0.00009641579,0.00009082474],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000091676695,0.000021631458,0.9618216,0.000050658622,0.000039084774,0.00015506255,0.0008220726,0.0022206844,0.0041720592,0.00021766288,0.00076878123,0.029619025],"study_design_scores_gemma":[0.0000041623944,0.000011024015,0.9942749,0.0000196337,0.000010915281,0.000039800983,0.00026690107,0.001348517,0.00047826333,0.000056295903,0.003486026,0.0000036031042],"about_ca_topic_score_codex":0.43075016,"about_ca_topic_score_gemma":0.4163568,"teacher_disagreement_score":0.43075016,"about_ca_system_score_codex":0.001557224,"about_ca_system_score_gemma":0.0011227583,"threshold_uncertainty_score":0.85648584},"labels":[],"label_agreement":null},{"id":"W2962948702","doi":"10.1029/2018jb016461","title":"The Effects of Earthquakes and Fluids on the Metamorphism of the Lower Continental Crust","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":99,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"European Research Council; Natural Environment Research Council; European Commission; Natural Sciences and Engineering Research Council of Canada; Norges Forskningsråd; Sight Research UK; Alexander von Humboldt-Stiftung","keywords":"Geology; Metamorphism; Crust; Continental crust; Metamorphic rock; Mylonite; Petrology; Shear zone; Continental collision; Lithology; Brittleness; Lithosphere; Slip (aerodynamics); Creep; Seismology; Tectonics; Geochemistry","score_opus":0.018498678158567053,"score_gpt":0.27102223589361657,"score_spread":0.25252355773504953,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2962948702","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99943167,0.00018894889,0.00002565624,0.000016849635,0.0000016864111,0.0000014086838,0.000045169436,0.00000267207,0.00028598672],"genre_scores_gemma":[0.9996824,0.00007676871,0.000016016329,0.0000072358057,0.0000020337754,8.1899145e-7,0.000041002782,9.67303e-7,0.0001727815],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999021,0.000032866395,0.000007545356,0.000013088132,0.000014730224,0.000029614208],"domain_scores_gemma":[0.99956757,0.00014582508,0.0001067568,0.000020371997,0.000049714938,0.00010980382],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018099013,0.00023756165,0.00020932111,0.00045153033,0.00018653214,0.00047489366,0.00012905116,0.00020498676,0.0017464603],"category_scores_gemma":[0.0007070545,0.0000986113,0.00022641581,0.00026034226,0.00033553896,0.00017900972,0.00036991743,0.00020080572,0.00017765583],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.008318412,0.00067018747,0.5736014,0.0002924439,0.00070125354,0.0014483031,0.0005771953,0.012701707,0.3461253,0.00059384125,0.00041875636,0.054551154],"study_design_scores_gemma":[0.00002366079,0.000580619,0.98924005,0.000010161328,0.00006788508,0.00011414381,0.00019006658,0.0022501696,0.00688199,0.00013574952,0.00049539836,0.0000100409725],"about_ca_topic_score_codex":0.0036242262,"about_ca_topic_score_gemma":0.0030927309,"teacher_disagreement_score":0.0036242262,"about_ca_system_score_codex":0.00031077993,"about_ca_system_score_gemma":0.00013418835,"threshold_uncertainty_score":0.007206261},"labels":[],"label_agreement":null},{"id":"W2963760717","doi":"10.1029/2019jb017336","title":"Seismotectonics of the Zagros (Iran) From Orogen‐Wide, Calibrated Earthquake Relocations","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":90,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"National Science Foundation","keywords":"Geology; Seismology; Induced seismicity; Seismotectonics; Active fault; Fault (geology); Crust; Sinistral and dextral; Geophysics","score_opus":0.0400281737295255,"score_gpt":0.2913132705724643,"score_spread":0.2512850968429388,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2963760717","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977708,0.000119791395,0.0001381875,0.000017752604,0.0000064089118,0.000008262651,0.0012169979,0.000016532435,0.0007052557],"genre_scores_gemma":[0.9951623,0.0001291354,0.00057839823,0.0000137651705,0.000012766703,0.00000644035,0.0038168624,0.000006697556,0.00027365616],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998375,0.000015532232,0.000017915037,0.00005480653,0.000037249265,0.000036899553],"domain_scores_gemma":[0.99975413,0.000015017783,0.00012122719,0.000040813615,0.000051059902,0.000017874208],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031990613,0.00027058492,0.00017771278,0.0015957018,0.00020864244,0.00036561093,0.0002613328,0.00020555593,0.0006740858],"category_scores_gemma":[0.0005297947,0.00010555653,0.00022079532,0.0018134406,0.00021317965,0.00019937275,0.0003774396,0.00017817937,0.0002668259],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021778757,0.00007363216,0.9451827,0.00008014533,0.00011803261,0.00034379287,0.0008134725,0.0033823987,0.0040479195,0.00020451116,0.0008895479,0.04464604],"study_design_scores_gemma":[0.000007949308,0.000013189465,0.99849,0.0000056630474,0.0000141524415,0.000047118112,0.00013734827,0.00034475306,0.00012606838,0.000012426115,0.00079834514,0.0000029705216],"about_ca_topic_score_codex":0.036102347,"about_ca_topic_score_gemma":0.059508543,"teacher_disagreement_score":0.036102347,"about_ca_system_score_codex":0.0005519363,"about_ca_system_score_gemma":0.00039508357,"threshold_uncertainty_score":0.07178444},"labels":[],"label_agreement":null},{"id":"W2964215184","doi":"10.1029/2018jb016382","title":"Gravity Gradiometry With GRACE Space Missions: New Opportunities for the Geosciences","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"York University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Gradiometer; Gravitational field; Geodesy; Gravity of Earth; Geology; Gravitation; Scale (ratio); Noise (video); Mode (computer interface); Geophysics; Computer science; Remote sensing; Physics; Geography; Cartography; Artificial intelligence; Classical mechanics","score_opus":0.13618862909784424,"score_gpt":0.3412065962855927,"score_spread":0.20501796718774845,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2964215184","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.22268116,0.0048517664,0.72590876,0.012936409,0.0009116477,0.00016269997,0.0028043687,0.00569886,0.024044374],"genre_scores_gemma":[0.68868434,0.0013043188,0.30475742,0.0007563994,0.0006407533,0.000114739276,0.0012440201,0.0005703605,0.0019276498],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99953055,0.00019952258,0.000017248074,0.000051873845,0.00016330888,0.00003746052],"domain_scores_gemma":[0.99869066,0.00031240302,0.00018343923,0.00041887068,0.0002303511,0.00016428887],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001692351,0.0005880721,0.00034403798,0.0008542443,0.00027776547,0.0015525876,0.00060682016,0.000484371,0.0015168547],"category_scores_gemma":[0.00319967,0.00020446167,0.00033172837,0.0012962735,0.0010014871,0.0018051071,0.0019164508,0.0011753903,0.00042097812],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00078585884,0.00024359787,0.07306219,0.0003317707,0.00038502537,0.00032318305,0.0007018436,0.06368207,0.058448274,0.13759084,0.026621636,0.63782376],"study_design_scores_gemma":[0.00023893022,0.0006482282,0.068066485,0.00028635064,0.00015548033,0.00048481408,0.00084425847,0.5708251,0.033326797,0.18349575,0.14129703,0.0003307507],"about_ca_topic_score_codex":0.0024063005,"about_ca_topic_score_gemma":0.0033043614,"teacher_disagreement_score":0.0024063005,"about_ca_system_score_codex":0.0003120072,"about_ca_system_score_gemma":0.0009142421,"threshold_uncertainty_score":0.008950114},"labels":[],"label_agreement":null},{"id":"W2964571751","doi":"10.1029/2019jb017643","title":"Detection of Low‐Frequency Earthquakes in Broadband Random Time Sequences: Are They Independent Events?","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Japan Society for the Promotion of Science; Natural Resources Canada; Ministry of Education, Culture, Sports, Science and Technology","keywords":"Seismogram; Waveform; Matched filter; Impulse (physics); Filter (signal processing); Acoustics; Broadband; Seismology; Physics; Sequence (biology); Geology; Algorithm; Computer science; Telecommunications; Optics","score_opus":0.022464943443949576,"score_gpt":0.2836457150635788,"score_spread":0.2611807716196292,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2964571751","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9373748,0.00021780896,0.060864825,0.00014693318,0.00003622023,0.000020368032,0.0000753545,0.000114055576,0.0011497742],"genre_scores_gemma":[0.99442554,0.000056079734,0.005242188,0.000015155462,0.0000138018895,0.0000046266355,0.000052122323,0.000010199757,0.00018028608],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997389,0.000053922806,0.000015650523,0.000070249094,0.0000842797,0.00003706127],"domain_scores_gemma":[0.9982968,0.0007324107,0.00050107465,0.00013774456,0.0002007435,0.00013127417],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008269319,0.00024779336,0.00034803708,0.0005749774,0.00013721417,0.0005320112,0.00039713073,0.0005963501,0.00093200355],"category_scores_gemma":[0.0047570644,0.00028093724,0.00026655183,0.00036747954,0.00037899017,0.00089826324,0.00026605697,0.00026362133,0.00022899087],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012953976,0.00042117215,0.33207187,0.00071313354,0.0005485216,0.0024648963,0.00052801316,0.19063659,0.291328,0.016816838,0.0011842367,0.16199125],"study_design_scores_gemma":[0.000068803834,0.00031142382,0.20649524,0.000057216246,0.00014957505,0.00080763025,0.00022588196,0.7546556,0.028883703,0.0070390785,0.0012364539,0.00006943108],"about_ca_topic_score_codex":0.00092817296,"about_ca_topic_score_gemma":0.0008583316,"teacher_disagreement_score":0.00093200355,"about_ca_system_score_codex":0.0002401517,"about_ca_system_score_gemma":0.00016237354,"threshold_uncertainty_score":0.0043732524},"labels":[],"label_agreement":null},{"id":"W2964649173","doi":"10.1029/2019jb017926","title":"Stability of Pulse‐Like Earthquake Ruptures","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Environment Research Council; Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; Sight Research UK","keywords":"Slip (aerodynamics); Perturbation (astronomy); Thermal; Cabin pressurization; Infinitesimal; Stress (linguistics); Steady state (chemistry)","score_opus":0.0448825337711925,"score_gpt":0.31570847695036763,"score_spread":0.27082594317917513,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2964649173","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99057686,0.000042927386,0.007077378,0.000086126835,0.0000067409583,0.00001077348,0.00008554433,0.0000619249,0.002051601],"genre_scores_gemma":[0.9992619,0.000014539581,0.00043463358,0.000008516996,0.0000013757536,0.000007791596,0.000045914843,0.000007030104,0.00021824133],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993026,0.000012567189,0.0000038287358,0.000017691269,0.000016004786,0.000019705607],"domain_scores_gemma":[0.99970067,0.00011426218,0.000060772563,0.000025840534,0.000052241394,0.000046333967],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021356373,0.00017357459,0.00030397737,0.00031858947,0.00032544235,0.0005906274,0.00041189793,0.0006053039,0.0012802478],"category_scores_gemma":[0.0013094312,0.00017732481,0.0003044133,0.00017352826,0.0005667039,0.00050597644,0.0004568567,0.00039905502,0.00009823018],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000110271474,0.00008366601,0.012235099,0.000036097175,0.00007091702,0.00024567483,0.0001257211,0.9566622,0.02017999,0.0063652326,0.00038817522,0.0034969854],"study_design_scores_gemma":[0.000009185951,0.000036195088,0.002596284,0.0000031850843,0.000005364325,0.000026910093,0.000029637573,0.99426997,0.0019817033,0.0009059001,0.00012889515,0.0000067624974],"about_ca_topic_score_codex":0.0024373666,"about_ca_topic_score_gemma":0.00080058386,"teacher_disagreement_score":0.0024373666,"about_ca_system_score_codex":0.0005562055,"about_ca_system_score_gemma":0.0003470284,"threshold_uncertainty_score":0.0048463345},"labels":[],"label_agreement":null},{"id":"W2965054426","doi":"10.1029/2019jb017589","title":"Micromechanical Behavior of DNA‐1A Lunar Regolith Simulant in Comparison to Ottawa Sand","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Granular flow and fluidized beds","field":"Engineering","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"City University of Hong Kong","keywords":"Regolith; Materials science; Surface roughness; Surface finish; Composite material; Discrete element method; Micromechanics; Geotechnical engineering; Contact angle; Indentation hardness; Mineralogy; Geology; Microstructure; Mechanics; Composite number; Physics","score_opus":0.027259082591981888,"score_gpt":0.3336621448507721,"score_spread":0.3064030622587902,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2965054426","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99917585,0.000075262586,0.00028794663,0.000006519067,0.0000023212237,0.000005551608,0.000119636316,0.000011294033,0.0003157],"genre_scores_gemma":[0.9983063,0.0000837403,0.000583208,0.00000463405,5.15515e-7,0.0000042610213,0.00014131978,0.000005154346,0.000870861],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998024,0.000012505533,0.000012456434,0.00004943662,0.00008802346,0.000035058092],"domain_scores_gemma":[0.9998282,0.000032326945,0.000035679215,0.000015138019,0.000057523917,0.00003102159],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014003195,0.0002244151,0.00024995857,0.00041423517,0.00025733377,0.00031343588,0.00026723658,0.00020002776,0.00092176645],"category_scores_gemma":[0.00026418897,0.00011807695,0.00017713284,0.0002799338,0.00034811426,0.00015664891,0.00021114542,0.00017451488,0.00016044635],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002135668,0.000024362278,0.0062163044,0.000056894824,0.000016008164,0.00016054114,0.00015878945,0.0013727393,0.9882763,0.000055463603,0.000038544098,0.0034104176],"study_design_scores_gemma":[0.000007715187,0.0005060385,0.054558516,0.0000076064252,0.000032433214,0.0001369152,0.0005230346,0.0043889126,0.93814445,0.00001962959,0.001651816,0.000022963215],"about_ca_topic_score_codex":0.025534727,"about_ca_topic_score_gemma":0.055592332,"teacher_disagreement_score":0.025534727,"about_ca_system_score_codex":0.00053573865,"about_ca_system_score_gemma":0.00038415054,"threshold_uncertainty_score":0.05077219},"labels":[],"label_agreement":null},{"id":"W2965950041","doi":"10.1029/2018jb017020","title":"Three‐Dimensional Sensitivity Kernels for Multicomponent Empirical Green's Functions From Ambient Noise: Methodology and Application to Adjoint Tomography","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Australian Research Council; Medical Research Council Canada; Macquarie University","keywords":"Tomography; Ambient noise level; Sensitivity (control systems); Noise (video); Kernel (algebra); Isotropy; Rotation (mathematics); Transverse plane; Acoustics; Physics; Mathematical analysis; Mathematics; Computer science; Geometry; Optics; Artificial intelligence","score_opus":0.07410705980697274,"score_gpt":0.35687408853777086,"score_spread":0.2827670287307981,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2965950041","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.03652031,0.00001963056,0.96276677,0.000030220172,0.0000054461066,0.000010978254,0.00001857023,0.00020298707,0.0004249907],"genre_scores_gemma":[0.77964693,0.000060374692,0.21941532,0.000025436726,0.000009640918,0.000040400588,0.00006633595,0.00010752838,0.00062795886],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998666,0.00004114996,0.000008102529,0.000016873259,0.000052333948,0.000014878917],"domain_scores_gemma":[0.9993774,0.0003312759,0.00007071968,0.00006150693,0.0001213727,0.00003770371],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00062748254,0.00039346362,0.0002095208,0.00065844326,0.00020981726,0.0006168219,0.0004868588,0.00038545078,0.0006406438],"category_scores_gemma":[0.0022510514,0.0002413133,0.00043388846,0.0004366452,0.0006707288,0.00066475326,0.0007488582,0.0005720685,0.00010588476],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000032501328,0.00005105327,0.0021140024,0.00003581005,0.000022028125,0.000100278645,0.00009712798,0.9185919,0.017170787,0.026810722,0.00024064981,0.034733117],"study_design_scores_gemma":[0.0000015198441,0.0000038360613,0.0001854457,0.0000015006997,0.0000012703072,0.000011932447,0.000005640355,0.9963182,0.0013186142,0.0020276573,0.00011958587,0.0000048105035],"about_ca_topic_score_codex":0.0032792466,"about_ca_topic_score_gemma":0.002366006,"teacher_disagreement_score":0.0032792466,"about_ca_system_score_codex":0.0004151903,"about_ca_system_score_gemma":0.00070956355,"threshold_uncertainty_score":0.006520331},"labels":[],"label_agreement":null},{"id":"W2966364567","doi":"10.1029/2018jb017153","title":"An Experimental Study on Effect of Boundary Condition on Particle Damage in Shear Zone of Crushed Sand","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geotechnical Engineering and Soil Mechanics","field":"Engineering","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Breakage; Shearing (physics); Void ratio; Geotechnical engineering; Materials science; Shear (geology); Void (composites); Particle (ecology); Direct shear test; Shear stress; Particle size; Composite material; Mechanics; Geology; Physics","score_opus":0.017512391376237953,"score_gpt":0.3399777320041124,"score_spread":0.32246534062787446,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2966364567","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996319,0.00003952061,0.00020819534,0.0000020493726,0.000002240971,0.0000046500513,0.000021888825,0.0000052840937,0.0000842052],"genre_scores_gemma":[0.9992374,0.000038720453,0.00041066046,0.000004524905,0.0000014596873,0.0000047059643,0.000050637813,0.0000034238285,0.0002485388],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9996939,0.000027838752,0.00002476514,0.00005860531,0.00012508953,0.000069763584],"domain_scores_gemma":[0.9994017,0.00017313687,0.00011172727,0.00008275348,0.00014636788,0.00008425729],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002888027,0.00030167663,0.00039457658,0.00029255028,0.00043902546,0.00019153228,0.00022997305,0.00036522406,0.0017748247],"category_scores_gemma":[0.0005151898,0.00019966703,0.00024424258,0.00016056832,0.00045990743,0.00023575789,0.0003039603,0.00037710834,0.00015078651],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004860106,0.000079343205,0.0023273467,0.00004824246,0.000008237568,0.00008602494,0.00011150092,0.00032269154,0.9950636,0.0000145573285,0.000011467596,0.0014410046],"study_design_scores_gemma":[0.000017655466,0.0024479527,0.035870824,0.000007748601,0.000022102928,0.00008973876,0.0001774054,0.002272869,0.95884305,0.000018579049,0.00021919388,0.000013020757],"about_ca_topic_score_codex":0.0020498713,"about_ca_topic_score_gemma":0.0031979429,"teacher_disagreement_score":0.0020498713,"about_ca_system_score_codex":0.00021824331,"about_ca_system_score_gemma":0.00015234516,"threshold_uncertainty_score":0.005937338},"labels":[],"label_agreement":null},{"id":"W2966859128","doi":"10.1029/2019jb018099","title":"Strain‐Dependent Rheology of Silicate Melt Foams: Importance for Outgassing of Silicic Lavas","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; University of British Columbia","funders":"H2020 Marie Skłodowska-Curie Actions; Natural Sciences and Engineering Research Council of Canada","keywords":"Outgassing; Materials science; Silicic; Rheology; Lava; Strain rate; Porosity; Composite material; Geology; Basalt; Volcano; Chemistry; Geochemistry","score_opus":0.04264037808114515,"score_gpt":0.3227758722224421,"score_spread":0.2801354941412969,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2966859128","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992471,0.00012246848,0.00024440087,0.000014201666,0.0000018174111,0.0000044068784,0.00009089018,0.00001604059,0.00025868535],"genre_scores_gemma":[0.9997639,0.000027638063,0.00009347287,0.0000045533207,0.0000010874056,0.0000028015033,0.00005525133,0.0000044596427,0.000046803136],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99989104,0.000010885561,0.000009992859,0.00002401528,0.000034815064,0.0000291985],"domain_scores_gemma":[0.9997292,0.00006184078,0.000075130454,0.000034816105,0.000056613095,0.000042392192],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015531848,0.00022536886,0.00027694413,0.0003143654,0.00020279002,0.00046101725,0.00021223375,0.00026310733,0.001085083],"category_scores_gemma":[0.00047058013,0.00015374098,0.00020435156,0.00014562563,0.00037963345,0.0003943,0.00021994057,0.00035468768,0.00009264411],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010712595,0.000018149123,0.008586622,0.000026257776,0.00001577691,0.000059396076,0.00008084648,0.00035534884,0.989571,0.00004917885,0.000017034048,0.0011131854],"study_design_scores_gemma":[0.000014369694,0.00031408112,0.14351259,0.000014104061,0.000023752726,0.0001655658,0.00026228925,0.012155378,0.8428547,0.00014003669,0.0005209543,0.000022194728],"about_ca_topic_score_codex":0.0013864462,"about_ca_topic_score_gemma":0.0011103109,"teacher_disagreement_score":0.0013864462,"about_ca_system_score_codex":0.00019211389,"about_ca_system_score_gemma":0.0001160576,"threshold_uncertainty_score":0.0036299229},"labels":[],"label_agreement":null},{"id":"W2967728354","doi":"10.1029/2018jb017260","title":"Nonmonotonic Postdeglacial Relative Sea Level Changes at the Aftermath of Marinoan (635 Ma) Snowball Earth Meltdown","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Natural Science Foundation of China; National Science Foundation","keywords":"Deglaciation; Geology; Snowball Earth; Marine transgression; Earth's rotation; Post-glacial rebound; Sedimentary rock; Sea level; Isostasy; Mantle (geology); Glacial period; Oceanography; Paleontology; Geodesy; Lithosphere; Tectonics","score_opus":0.049532699075074106,"score_gpt":0.31782404448174695,"score_spread":0.2682913454066728,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2967728354","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988232,0.000066311084,0.000060715458,0.00004523666,0.000005468369,0.0000019332501,0.00026276134,0.000026347185,0.00070800923],"genre_scores_gemma":[0.99947506,0.000023537821,0.000030156394,0.000010159809,0.0000034796747,0.0000013743066,0.0002850676,0.000003982343,0.0001671242],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995303,0.0000025766146,0.000003496898,0.000017768709,0.0000080945565,0.000015037541],"domain_scores_gemma":[0.99983454,0.000013750482,0.00004060569,0.000013685515,0.000050969862,0.00004640031],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016306103,0.0002584173,0.00023608358,0.0008138008,0.00052959786,0.0005787241,0.0002680925,0.00032704385,0.0016287024],"category_scores_gemma":[0.00045400768,0.00018762864,0.00033086608,0.00057630264,0.0003515569,0.0002517807,0.00047038813,0.00023938996,0.00022616617],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024667277,0.000026723665,0.9612758,0.000037981044,0.00011968529,0.00037287685,0.00056381634,0.002041294,0.028445825,0.00017267946,0.0004533322,0.0062432117],"study_design_scores_gemma":[0.000003399809,0.000010981375,0.99822766,0.0000023047342,0.000009688803,0.000012485002,0.000072680035,0.0009344796,0.00041742742,0.000015025458,0.00029036767,0.000003535134],"about_ca_topic_score_codex":0.1078373,"about_ca_topic_score_gemma":0.12957025,"teacher_disagreement_score":0.1078373,"about_ca_system_score_codex":0.0010987049,"about_ca_system_score_gemma":0.0005194452,"threshold_uncertainty_score":0.21441919},"labels":[],"label_agreement":null},{"id":"W2968045198","doi":"10.1029/2019jb017713","title":"Pyroxene <sup>40</sup>Ar/<sup>39</sup>Ar Dating of Basalt and Applications to Large Igneous Provinces and Precambrian Stratigraphic Correlations","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Fundamental Research Funds for the Central Universities; Australian Research Council; Geological Survey of Western Australia; State Key Laboratory of Geological Processes and Mineral Resources; National Natural Science Foundation of China","keywords":"Geology; Basalt; Precambrian; Igneous rock; Pyroxene; Large igneous province; Flood basalt; Geochemistry; Mafic; Deccan Traps; Felsic; Volcanic rock; Geochronology; Lava; Paleontology; Volcano; Magmatism; Volcanism; Olivine","score_opus":0.01965291012017235,"score_gpt":0.2789824011761705,"score_spread":0.2593294910559982,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2968045198","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98131335,0.0011559718,0.0068401597,0.000044064018,0.000011810482,0.0000428154,0.0007509383,0.00014565603,0.009695328],"genre_scores_gemma":[0.98752624,0.00046535878,0.008130825,0.000014825221,0.000005584891,0.000015918888,0.0004920606,0.000050441933,0.0032986389],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99967563,0.000036219797,0.000026640613,0.0000857426,0.00014496986,0.000030777064],"domain_scores_gemma":[0.99965703,0.0000489876,0.00008685236,0.000058566384,0.00013404406,0.000014517503],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005341468,0.00026354368,0.00019795343,0.0012698893,0.00027998426,0.00058389147,0.00034052183,0.00019382965,0.001970178],"category_scores_gemma":[0.0005192148,0.00019791379,0.00017897847,0.00070602464,0.00032699615,0.00019123995,0.0003223228,0.00020271598,0.0006680924],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020143387,0.000036488374,0.14182572,0.00021965531,0.00010484552,0.0006040118,0.0005964417,0.0033325667,0.78425694,0.000767686,0.0003574584,0.06769685],"study_design_scores_gemma":[0.00000775365,0.0001143911,0.8134196,0.00003850222,0.000051397703,0.00071600266,0.00021879748,0.008788773,0.1660245,0.0003691727,0.010230367,0.00002080068],"about_ca_topic_score_codex":0.013264198,"about_ca_topic_score_gemma":0.033390272,"teacher_disagreement_score":0.013264198,"about_ca_system_score_codex":0.00032081446,"about_ca_system_score_gemma":0.0003257186,"threshold_uncertainty_score":0.026373982},"labels":[],"label_agreement":null},{"id":"W2968268494","doi":"10.1029/2019jb017419","title":"Interseismic Quiescence and Triggered Slip of Active Normal Faults of Kīlauea Volcano's South Flank During 2001–2018","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Golder Associates (Canada)","funders":"University of California Berkeley; National Aeronautics and Space Administration","keywords":"Geology; Seismology; Flank; Interferometric synthetic aperture radar; Volcano; Slip (aerodynamics); Rift zone; Geodesy; Fault (geology); Rift; Tectonics; Synthetic aperture radar; Remote sensing; Anatomy","score_opus":0.029393306890855595,"score_gpt":0.2894609964926335,"score_spread":0.2600676896017779,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2968268494","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992273,0.000038743776,0.000017646711,0.000015802772,0.00000276693,0.000001909893,0.00036052626,0.0000045580264,0.00033081573],"genre_scores_gemma":[0.9988844,0.000038244012,0.00005081339,0.000006935925,0.000007018339,0.0000040856175,0.0007256874,0.0000017628754,0.00028105197],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999186,0.000005576527,0.0000062671684,0.00002405523,0.000022902454,0.00002257925],"domain_scores_gemma":[0.9997048,0.000022407401,0.00012841383,0.000015679256,0.00006833197,0.000060333467],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015329657,0.00021895341,0.00016112799,0.0007593369,0.00029131921,0.0003884499,0.0002217335,0.0001671501,0.00087027374],"category_scores_gemma":[0.0005170526,0.00010375622,0.00012168208,0.00057459145,0.00026101258,0.00026154393,0.0003346032,0.00016565625,0.00014463105],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001296058,0.000043660293,0.9822397,0.0000418907,0.000045161454,0.00042118778,0.0013954934,0.0003642293,0.0066369846,0.00006140827,0.000569054,0.008051587],"study_design_scores_gemma":[0.0000012109356,0.0000100211455,0.9991999,0.0000033735985,0.000003763155,0.000026702728,0.0001822859,0.00015667998,0.00012313583,0.0000043544755,0.0002873424,0.0000012753976],"about_ca_topic_score_codex":0.037006237,"about_ca_topic_score_gemma":0.088997856,"teacher_disagreement_score":0.037006237,"about_ca_system_score_codex":0.0006136134,"about_ca_system_score_gemma":0.00032868987,"threshold_uncertainty_score":0.073581636},"labels":[],"label_agreement":null},{"id":"W2970129466","doi":"10.1029/2019jb017741","title":"Modification of the Seismic Properties of Subducting Continental Crust by Eclogitization and Deformation Processes","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"Deutsche Forschungsgemeinschaft","keywords":"Geology; Eclogitization; Subduction; Granulite; Seismic anisotropy; Crust; Eclogite; Seismology; Protolith; Geophysics; Structural geology; Continental crust; Continental collision; Petrology; Facies; Mantle (geology); Tectonics; Geomorphology; Oceanic crust","score_opus":0.032906883136148445,"score_gpt":0.2587077701664769,"score_spread":0.22580088703032844,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2970129466","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994023,0.00003448532,0.00015706915,0.0000014601231,4.2930037e-7,0.0000016804375,0.000088794106,0.000002952023,0.00031074788],"genre_scores_gemma":[0.9995468,0.000028025961,0.0001864141,0.0000018743017,5.931585e-7,0.000001977276,0.00013357234,0.0000022976626,0.000098434386],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992836,0.000008403821,0.000006917873,0.000029132305,0.000012682992,0.000014588681],"domain_scores_gemma":[0.9998926,0.00002095147,0.000039103023,0.000009136614,0.000022436288,0.000015822872],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011276511,0.0002492608,0.00012484775,0.0009817609,0.00016517234,0.00048680938,0.00016508135,0.00014800334,0.0009022708],"category_scores_gemma":[0.00032932093,0.00017356647,0.00009297652,0.0007080741,0.0005540116,0.00020150328,0.0003239457,0.000100015735,0.00012850546],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017734342,0.000031422613,0.8085407,0.00005524294,0.00004311007,0.00029206352,0.0009471539,0.0016407944,0.1770269,0.0001468341,0.000034225708,0.011064174],"study_design_scores_gemma":[0.000001849591,0.00001794547,0.9980357,0.000001934508,0.0000032722544,0.000044424443,0.000103003775,0.00038296886,0.0012979005,0.000015241412,0.00009417741,0.00000149387],"about_ca_topic_score_codex":0.009470059,"about_ca_topic_score_gemma":0.012923563,"teacher_disagreement_score":0.009470059,"about_ca_system_score_codex":0.0003401964,"about_ca_system_score_gemma":0.00014899681,"threshold_uncertainty_score":0.018829823},"labels":[],"label_agreement":null},{"id":"W2980364451","doi":"10.1029/2019jb017944","title":"The Effects of Shear Strain, Fabric, and Porosity Evolution on Elastic and Mechanical Properties of Clay‐Rich Fault Gouge","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"National Stroke Foundation; U.S. Department of Energy; Office of Energy Efficiency and Renewable Energy; National Science Foundation","keywords":"Porosity; Shear (geology); Materials science; Fault gouge; Shearing (physics); Composite material; Elastic modulus; Stiffness; Shear modulus; Shear zone; Shear stress; Geotechnical engineering; Geology; Fault (geology)","score_opus":0.02119352155678692,"score_gpt":0.26884891755047097,"score_spread":0.24765539599368405,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2980364451","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99980646,0.000024118779,0.000066968125,0.0000022491156,5.4920974e-7,0.0000012734472,0.000030621813,0.0000030668764,0.00006457273],"genre_scores_gemma":[0.99981624,0.000014917281,0.00007397365,0.0000020437524,3.043093e-7,0.0000018084896,0.000031855932,0.0000015725369,0.000057233214],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998925,0.000011767815,0.000009480255,0.000024551226,0.000031199022,0.00003043694],"domain_scores_gemma":[0.99970514,0.00007542111,0.00010089255,0.00002032227,0.000045695593,0.000052550335],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001998779,0.00022896793,0.00015273527,0.00033410496,0.0001657931,0.00034161634,0.00013007411,0.00016863072,0.0007157288],"category_scores_gemma":[0.00041564312,0.00014420871,0.00010717242,0.00017503682,0.00039153104,0.00019884706,0.00019836475,0.00023140517,0.00006103498],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013989277,0.000017549251,0.0051017916,0.000022969054,0.000010276531,0.000058168403,0.00004926158,0.000586128,0.99304295,0.00003350163,0.000014069332,0.00092338613],"study_design_scores_gemma":[0.00001199252,0.0003627181,0.12511131,0.000008762577,0.000016161588,0.000102886814,0.00023522071,0.006141825,0.867631,0.000043470478,0.0003154982,0.000019210636],"about_ca_topic_score_codex":0.0016267124,"about_ca_topic_score_gemma":0.0022287988,"teacher_disagreement_score":0.0016267124,"about_ca_system_score_codex":0.00023556486,"about_ca_system_score_gemma":0.000108239095,"threshold_uncertainty_score":0.0032345057},"labels":[],"label_agreement":null},{"id":"W2981631412","doi":"10.1029/2019jb017875","title":"The Significance of Tomographic Edge Zones for Large Earthquakes in Taiwan","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"National Natural Science Foundation of China-Yunnan Joint Fund; Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Seismology; Tectonics; Seismotectonics; Seismic tomography; Crust; Geophysics; Mantle (geology)","score_opus":0.03307738090649209,"score_gpt":0.3163455562020572,"score_spread":0.2832681752955651,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2981631412","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994006,0.000035975394,0.00017237356,0.0000135126365,0.0000011095647,0.0000018734792,0.00010108908,0.000013309653,0.0002602058],"genre_scores_gemma":[0.9997582,0.000011172646,0.000072827715,0.0000024145518,0.0000015233094,8.995861e-7,0.00012033316,0.0000016753864,0.00003090538],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998877,0.000013449896,0.0000122364745,0.000035165052,0.000018183135,0.000033170923],"domain_scores_gemma":[0.99928916,0.00010971149,0.0003274487,0.0000643858,0.000110450244,0.00009880256],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021974587,0.00018466038,0.00014864815,0.0015047817,0.00022251181,0.00055943493,0.00022653672,0.00025978588,0.0007878997],"category_scores_gemma":[0.0010376805,0.00016373052,0.00019645557,0.0010846737,0.00024170177,0.00031872344,0.0006037612,0.00018363954,0.00014408074],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000067087705,0.00001739148,0.9864624,0.000014224013,0.000019375526,0.00020487161,0.00016762741,0.001062376,0.005372714,0.0000527849,0.00008614569,0.0064730155],"study_design_scores_gemma":[0.000003421336,0.000011670883,0.99621767,0.0000048259526,0.000011622945,0.000116557625,0.00019890678,0.0028420018,0.00041728132,0.000035371308,0.00013533795,0.0000053117888],"about_ca_topic_score_codex":0.0066462546,"about_ca_topic_score_gemma":0.008992263,"teacher_disagreement_score":0.0066462546,"about_ca_system_score_codex":0.00018387275,"about_ca_system_score_gemma":0.0002012642,"threshold_uncertainty_score":0.013215125},"labels":[],"label_agreement":null},{"id":"W2988563457","doi":"10.1029/2019jb018653","title":"Influence of Upper Plate Structure on Flat‐Slab Depth: Numerical Modeling of Subduction Dynamics","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Slab; Geology; Slab window; Subduction; Lithosphere; Craton; Mantle (geology); Seismology; Petrology; Geophysics; Oceanic crust; Tectonics","score_opus":0.019609645710791965,"score_gpt":0.2920404882237749,"score_spread":0.2724308425129829,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2988563457","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9740617,0.00023511033,0.012672944,0.00044309295,0.00004702937,0.000049415787,0.00040485561,0.00020512828,0.011880648],"genre_scores_gemma":[0.9953752,0.00009530254,0.0027789837,0.00004755038,0.000012124715,0.00004869555,0.000113743714,0.000026799966,0.0015016642],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998671,0.000048449318,0.0000072046523,0.000022571327,0.00002102363,0.000033798664],"domain_scores_gemma":[0.9993299,0.00038432892,0.0000957124,0.00003591043,0.00007800979,0.00007619121],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004223492,0.0007690958,0.0007001868,0.00055801624,0.000755171,0.0015598135,0.0009200651,0.0017453558,0.0019890005],"category_scores_gemma":[0.0015425121,0.0006042649,0.00087630894,0.00045963418,0.0010870778,0.00063624274,0.0007893874,0.00076563365,0.00020141147],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017302276,0.0000142762765,0.0012350553,0.0000044756503,0.000009174948,0.000020654052,0.000010942129,0.9977324,0.00028788488,0.0003253436,0.000038503844,0.00030388642],"study_design_scores_gemma":[0.000005860818,0.0000068288773,0.00024808574,0.0000014588172,0.000002180435,0.0000017099242,0.000006093345,0.99952984,0.000051732513,0.00010261341,0.000041457708,0.000002163797],"about_ca_topic_score_codex":0.05832182,"about_ca_topic_score_gemma":0.019869125,"teacher_disagreement_score":0.05832182,"about_ca_system_score_codex":0.0014562863,"about_ca_system_score_gemma":0.0011374506,"threshold_uncertainty_score":0.11596471},"labels":[],"label_agreement":null},{"id":"W2990280149","doi":"10.1029/2019jb018324","title":"Strength of Laboratory Synthesized Hydrate‐Bearing Sands and Their Relationship to Natural Hydrate‐Bearing Sediments","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Cohesion (chemistry); Hydrate; Saturation (graph theory); Geotechnical engineering; Particle size; Materials science; Porosity; Geology; Softening; Effective stress; Particle (ecology); Mineralogy; Composite material; Chemistry","score_opus":0.02087484907797423,"score_gpt":0.2945645159166441,"score_spread":0.2736896668386699,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2990280149","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99856037,0.00011861125,0.00055638567,0.0000073773963,0.0000034376528,0.000009268679,0.00026486817,0.000018155326,0.00046156047],"genre_scores_gemma":[0.9990947,0.0000643952,0.00038819795,0.0000054670913,0.0000010801034,0.0000114386,0.00015513183,0.000005836953,0.00027365336],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99983513,0.00001414561,0.000019324174,0.000038727034,0.00006991778,0.000022729373],"domain_scores_gemma":[0.99959725,0.000081311235,0.000128862,0.000021169573,0.00011342289,0.0000580672],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023267262,0.00024501252,0.00016673066,0.00053748843,0.00017120744,0.0002389658,0.00021987788,0.00017885683,0.0010695532],"category_scores_gemma":[0.00048700385,0.00024637516,0.00016340331,0.0003471874,0.00036174778,0.000123243,0.00018837597,0.0002244262,0.000089422385],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015199628,0.000026441774,0.0067744,0.00008699525,0.000026405663,0.000103035,0.0000959427,0.0014576635,0.9894174,0.0000909658,0.000029587018,0.0017391595],"study_design_scores_gemma":[0.000009787179,0.0002185046,0.06394064,0.000011195668,0.00003120282,0.000085071864,0.00022836408,0.0032944004,0.93151766,0.000034419736,0.000611561,0.000017226543],"about_ca_topic_score_codex":0.0032688878,"about_ca_topic_score_gemma":0.0077882446,"teacher_disagreement_score":0.0032688878,"about_ca_system_score_codex":0.00045239454,"about_ca_system_score_gemma":0.00019169488,"threshold_uncertainty_score":0.0064997673},"labels":[],"label_agreement":null},{"id":"W2990757039","doi":"10.1029/2020jb020606","title":"Statistical Modeling and Characterization of Induced Seismicity Within the Western Canada Sedimentary Basin","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Induced seismicity; Aftershock; Seismology; Geology; Tectonics; Magnitude (astronomy); Structural basin; Maximum magnitude; Sedimentary rock; Paleontology","score_opus":0.057131941164127065,"score_gpt":0.2925628592753173,"score_spread":0.2354309181111902,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2990757039","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962961,0.00003123584,0.0023710197,0.000039806724,0.0000019240586,0.000015836076,0.0007133388,0.000029697458,0.00050097785],"genre_scores_gemma":[0.99819237,0.000028301347,0.0005577588,0.000004122287,0.0000013755897,0.000005735851,0.0008248397,0.0000037598336,0.00038167852],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997031,0.00003664803,0.00002108485,0.000074749216,0.0000922032,0.0000720878],"domain_scores_gemma":[0.9988932,0.00033941574,0.00017746096,0.00009033322,0.00039791997,0.00010165177],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004972803,0.00021480396,0.00019956009,0.0013540031,0.0005572073,0.0006812857,0.0006223989,0.00018353503,0.000842371],"category_scores_gemma":[0.0028607666,0.00014034167,0.00037574777,0.0014713941,0.0005324198,0.0001957891,0.00035792938,0.00026918258,0.00007672396],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000104353676,0.000051970568,0.80300856,0.00002645456,0.00020189266,0.00026467466,0.00029583613,0.17406294,0.0018674253,0.0016278842,0.00083134155,0.017656662],"study_design_scores_gemma":[0.000005251126,0.000029498107,0.6381572,0.0000073853093,0.000038830407,0.000037443762,0.00049427745,0.35945603,0.00048834406,0.00042723498,0.00084141793,0.000017110238],"about_ca_topic_score_codex":0.92724866,"about_ca_topic_score_gemma":0.90603936,"teacher_disagreement_score":0.07275134,"about_ca_system_score_codex":0.0048495177,"about_ca_system_score_gemma":0.0045939963,"threshold_uncertainty_score":0.1463595},"labels":[],"label_agreement":null},{"id":"W2991346486","doi":"10.1029/2019jb018121","title":"Insights From Micromechanical Modeling of Intact Rock Failure: Event Characteristics, Stress Drops, and Force Networks","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Rock Mechanics and Modeling","field":"Engineering","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Brittleness; Acoustic emission; Stress (linguistics); Deformation (meteorology); Mechanics; Observable; Materials science; Strain rate; Differential stress; Geology; Physics; Composite material","score_opus":0.015724689313960833,"score_gpt":0.2675785911456672,"score_spread":0.25185390183170636,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2991346486","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93632543,0.0000746648,0.06105004,0.000079323,0.0000082662045,0.000038319522,0.00015802575,0.00015114398,0.0021146839],"genre_scores_gemma":[0.9958046,0.000035733177,0.003653948,0.0000067409546,0.0000031496745,0.00002183336,0.00003862208,0.00001950783,0.00041577965],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99990964,0.000016841223,0.000005702593,0.00002007755,0.000029951374,0.00001774298],"domain_scores_gemma":[0.9996234,0.00017817713,0.00006870244,0.00005052431,0.00004306006,0.00003607161],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035041937,0.00034867157,0.00028813467,0.00062458456,0.0002954505,0.00039876864,0.0007303339,0.0007063103,0.0014200183],"category_scores_gemma":[0.000870659,0.00035896787,0.00031032873,0.0002385499,0.0004642305,0.0005602585,0.00020864006,0.00039093653,0.0001870645],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000036122397,0.00007660111,0.009502198,0.00002582822,0.000019779722,0.00016992331,0.000077339624,0.96389174,0.020629792,0.0010954111,0.000099834964,0.004375367],"study_design_scores_gemma":[0.0000015672576,0.0000120115,0.0017441316,9.1659234e-7,0.0000015209995,0.000010616603,0.0000068359946,0.99722505,0.000756841,0.00019588723,0.000041680873,0.0000030487035],"about_ca_topic_score_codex":0.006185816,"about_ca_topic_score_gemma":0.0043064607,"teacher_disagreement_score":0.006185816,"about_ca_system_score_codex":0.0005169077,"about_ca_system_score_gemma":0.0003820287,"threshold_uncertainty_score":0.012299657},"labels":[],"label_agreement":null},{"id":"W2994772960","doi":"10.1029/2019jb018132","title":"Support Vector Machine Classification of Seismic Events in the Tianshan Orogenic Belt","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Natural Science Foundation of China","keywords":"Geology; Seismology; Support vector machine; Tectonics; Aftershock; Linear discriminant analysis; Event (particle physics); Machine learning; Artificial intelligence","score_opus":0.04838211000766522,"score_gpt":0.32810722610715076,"score_spread":0.2797251160994855,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2994772960","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996609,0.000052533822,0.002674729,0.000037147085,0.00001073975,0.000009509702,0.00025085057,0.000038525683,0.00031705675],"genre_scores_gemma":[0.99818784,0.000017865039,0.0011695332,0.0000054043244,0.000006238381,0.000004807072,0.00045613648,0.0000010553756,0.0001511616],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997925,0.00003923107,0.00003092115,0.000047139773,0.000050936767,0.000039376202],"domain_scores_gemma":[0.99954706,0.0001249361,0.00012560654,0.000030085486,0.000118864176,0.000053344964],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041280617,0.00030266913,0.0002447587,0.0015548206,0.00012547444,0.00029341815,0.00028670835,0.00021722462,0.0005394254],"category_scores_gemma":[0.00095256965,0.000060744773,0.00020809866,0.00090912957,0.00012455141,0.00024158564,0.00019240483,0.00014549377,0.00015583161],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005969606,0.00029748396,0.6780507,0.00010622656,0.00010649048,0.0006173182,0.00021413298,0.04336879,0.023001736,0.00040309923,0.0023118097,0.2509253],"study_design_scores_gemma":[0.000028162212,0.0001837726,0.4682947,0.000016056905,0.000042440937,0.000104706385,0.0002949915,0.52504677,0.0049710777,0.0003109154,0.0006868859,0.000019557241],"about_ca_topic_score_codex":0.005704698,"about_ca_topic_score_gemma":0.004021206,"teacher_disagreement_score":0.005704698,"about_ca_system_score_codex":0.000291683,"about_ca_system_score_gemma":0.00023461583,"threshold_uncertainty_score":0.011343002},"labels":[],"label_agreement":null},{"id":"W2994977238","doi":"10.1029/2019jb018680","title":"Calculating Effective Elastic Properties of Berea Sandstone Using the Segmentation‐Less Method Without Targets","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Mineralogy","score_opus":0.08396850352801277,"score_gpt":0.36259253777711836,"score_spread":0.2786240342491056,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2994977238","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.24709463,0.0001662463,0.7448033,0.000107497624,0.000048055143,0.00007560459,0.0003518738,0.004006748,0.003346091],"genre_scores_gemma":[0.6561222,0.00008154334,0.34095198,0.000059016336,0.0000128394795,0.000070643204,0.000584306,0.00034323108,0.0017742298],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997639,0.000025795729,0.000019969053,0.000045442393,0.00012424793,0.00002057745],"domain_scores_gemma":[0.999527,0.00015997759,0.000069111375,0.00008561962,0.000126369,0.00003191829],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040461085,0.00059497874,0.00037415035,0.0010205198,0.0003059594,0.00069614535,0.0007296187,0.0007613182,0.0014990609],"category_scores_gemma":[0.0013867471,0.00043003637,0.0005475821,0.00056116254,0.00037992618,0.0006580132,0.00047377052,0.00035965894,0.00042500778],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003173623,0.00018226028,0.017670305,0.00026850915,0.00012891812,0.0002669104,0.00023898989,0.63598627,0.15667342,0.0043106377,0.001439424,0.18251698],"study_design_scores_gemma":[0.000011267097,0.000026807309,0.0028321291,0.000008355614,0.00000997061,0.000055189037,0.000016352087,0.9759807,0.019751703,0.00047263686,0.0008153386,0.000019511514],"about_ca_topic_score_codex":0.0075682933,"about_ca_topic_score_gemma":0.0107387435,"teacher_disagreement_score":0.0075682933,"about_ca_system_score_codex":0.00045817878,"about_ca_system_score_gemma":0.00097381044,"threshold_uncertainty_score":0.015048504},"labels":[],"label_agreement":null},{"id":"W2997237258","doi":"10.1029/2019jb018739","title":"Three‐Dimensional Surface Displacements During the 2016 <i>M</i><sub><i>W</i></sub> 7.8 Kaikōura Earthquake (New Zealand) From Photogrammetry‐Derived Point Clouds","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Geology; Slip (aerodynamics); Seismology; Fault (geology); Geodesy; Surface rupture; Lidar; Earthquake rupture; Geometry; Remote sensing; Engineering","score_opus":0.031706971082110666,"score_gpt":0.27289218701218165,"score_spread":0.24118521593007097,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2997237258","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9869942,0.000050372375,0.0008033772,0.000044188317,0.000016961156,0.00003991861,0.00986302,0.00016809425,0.0020198904],"genre_scores_gemma":[0.9804388,0.000111492554,0.0022639956,0.000015485137,0.000011542539,0.00006290625,0.01604742,0.00002769508,0.0010206058],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99982953,0.00000451836,0.000011277758,0.00004667222,0.00007561855,0.00003237154],"domain_scores_gemma":[0.9997255,0.00001593429,0.00008065612,0.00002767791,0.00009910073,0.00005096664],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013028985,0.0004976559,0.00035031402,0.0009967824,0.0003209974,0.00068705285,0.00036916442,0.0003921655,0.0018635261],"category_scores_gemma":[0.0005803284,0.0002858865,0.00049591565,0.00166488,0.0003217999,0.00051612686,0.0007274218,0.0003459436,0.0008120698],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00075266307,0.00029874837,0.77217054,0.00039903022,0.00031635835,0.0009810105,0.0022717395,0.04951611,0.060133256,0.00035409682,0.010240744,0.10256582],"study_design_scores_gemma":[0.000022284441,0.000043779408,0.9794194,0.00002483573,0.000029716597,0.00006903691,0.0004155408,0.016571032,0.0016338589,0.00004292003,0.0016890963,0.000038477705],"about_ca_topic_score_codex":0.1676022,"about_ca_topic_score_gemma":0.26914352,"teacher_disagreement_score":0.1676022,"about_ca_system_score_codex":0.0007723041,"about_ca_system_score_gemma":0.000719341,"threshold_uncertainty_score":0.33325326},"labels":[],"label_agreement":null},{"id":"W2997479603","doi":"10.1029/2019jb018333","title":"ITRF2014, Earth Figure Changes, and Geocenter Velocity: Implications for GIA and Recent Ice Melting","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"University of Toronto; Institut de Physique du Globe de Paris; Centre National d’Etudes Spatiales; Natural Environment Research Council; Sight Research UK","keywords":"Post-glacial rebound; Geodesy; Geology; Geoid; Satellite geodesy; Spherical harmonics; Mantle (geology); Geophysics; Physics; Glacial period; Geodetic datum; Geomorphology","score_opus":0.12234947016138485,"score_gpt":0.34112950365976186,"score_spread":0.218780033498377,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2997479603","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98456687,0.00036125645,0.0025685488,0.00018089914,0.000055124678,0.000015678219,0.0058783595,0.0002260379,0.006147234],"genre_scores_gemma":[0.99413353,0.000105111416,0.0009532737,0.000011727373,0.000018887018,0.0000059104227,0.0043710573,0.00005508308,0.00034550962],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99980015,0.000027831704,0.00001652278,0.000051072282,0.00005572659,0.000048612685],"domain_scores_gemma":[0.99940264,0.00006972051,0.0002136302,0.00008883598,0.00017135705,0.00005385488],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00063199655,0.0003041119,0.00021959045,0.0016149769,0.00021614697,0.0007309226,0.00030924423,0.00036667884,0.0014614391],"category_scores_gemma":[0.0021911073,0.0001511265,0.0005012937,0.0022039677,0.00029694068,0.00054659,0.00044367605,0.00033251516,0.00038021768],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002119839,0.00004861607,0.90378016,0.00012927051,0.00016041142,0.0002134168,0.0002987953,0.052923374,0.0035991375,0.0017010261,0.0043367934,0.03259696],"study_design_scores_gemma":[0.000008064228,0.000015018949,0.9672965,0.000023938266,0.00003222521,0.000041343905,0.00012246911,0.027753528,0.0011166688,0.0002845844,0.0032868695,0.000018865221],"about_ca_topic_score_codex":0.058605175,"about_ca_topic_score_gemma":0.04746047,"teacher_disagreement_score":0.058605175,"about_ca_system_score_codex":0.0011615067,"about_ca_system_score_gemma":0.00053743954,"threshold_uncertainty_score":0.116528094},"labels":[],"label_agreement":null},{"id":"W2997952198","doi":"10.1029/2019jb018837","title":"The Upper Mantle Structure of Northwestern Canada From Teleseismic Body Wave Tomography","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Yukon University; Geological Survey of Canada; Natural Resources Canada; University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada; Ontario Ministry of Research, Innovation and Science","keywords":"Lithosphere; Geology; Craton; Seismology; Mantle (geology); Collision zone; Seismic tomography; Thrust fault; Crust; Geophysics; Tectonics","score_opus":0.018975202818169223,"score_gpt":0.25164305819732513,"score_spread":0.2326678553791559,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2997952198","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9822588,0.00034348472,0.0019544729,0.00023683577,0.000010060274,0.000025646776,0.0069304965,0.00030419248,0.007936013],"genre_scores_gemma":[0.9924602,0.00026177353,0.0019831746,0.000029789902,0.0000035549626,0.0000075599028,0.0031518498,0.000041674026,0.0020603717],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992967,0.0000014441517,0.0000020986572,0.000011283729,0.000032319964,0.000023174269],"domain_scores_gemma":[0.99985313,0.000010141721,0.000013547213,0.000006349899,0.000095497024,0.000021317433],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007841874,0.00042398638,0.00012753278,0.0015561826,0.0007588776,0.001163751,0.00041908884,0.00031222295,0.0025514257],"category_scores_gemma":[0.00036681222,0.00021034607,0.00018554216,0.002591778,0.00027014257,0.00020757293,0.00041063808,0.00024279032,0.00028863671],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00060607644,0.00012300913,0.64267963,0.0001832698,0.00023118475,0.0017344885,0.0016977681,0.05843583,0.11111804,0.0043745465,0.011758347,0.16705787],"study_design_scores_gemma":[0.000042755077,0.000018928391,0.9130772,0.000046747442,0.00009523054,0.00022526098,0.00091006863,0.06877148,0.008213851,0.0005556224,0.007986345,0.000056464163],"about_ca_topic_score_codex":0.9698953,"about_ca_topic_score_gemma":0.9835523,"teacher_disagreement_score":0.030104697,"about_ca_system_score_codex":0.0058477563,"about_ca_system_score_gemma":0.008122193,"threshold_uncertainty_score":0.060563922},"labels":[],"label_agreement":null},{"id":"W2998474489","doi":"10.1029/2019jb018378","title":"A Block Model of Present‐Day Kinematics of Alaska and Western Canada","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":111,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation of Sri Lanka; U.S. Geological Survey","keywords":"Geology; Seismology; Subduction; North American Plate; Forearc; Slab; Clockwise; Plate tectonics; Tectonics; Euler's rotation theorem; Pacific Plate; Block (permutation group theory); Geodesy; Paleontology; Rotation (mathematics); Geometry","score_opus":0.06236617944763835,"score_gpt":0.298615024653556,"score_spread":0.23624884520591766,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2998474489","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7839274,0.00080731325,0.1304899,0.0010722524,0.00012518499,0.0001275798,0.0054736915,0.0005964922,0.07738014],"genre_scores_gemma":[0.96329135,0.00049465237,0.0065917424,0.00004185653,0.00001735134,0.000105476065,0.0010479331,0.0000693486,0.028340338],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992967,0.0000089997,0.0000029606367,0.000017424956,0.000018261824,0.000022677086],"domain_scores_gemma":[0.99986124,0.000022144828,0.000021913484,0.00000948165,0.000053693442,0.000031569445],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016139077,0.00045216092,0.00039370806,0.0006096494,0.0011074644,0.0010356328,0.0014928529,0.0007036411,0.0054036314],"category_scores_gemma":[0.00054702885,0.00043377993,0.00045519546,0.0007311225,0.000793066,0.0006856975,0.00046301383,0.00046940765,0.00076843385],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023993882,0.000006700654,0.0029828853,0.000007210573,0.00001137063,0.000054844346,0.000066926295,0.98124665,0.00032879913,0.01254739,0.00067015464,0.0020530114],"study_design_scores_gemma":[0.000012748632,0.000006719415,0.0012639606,0.0000048453644,0.000008654692,0.0000118955495,0.000029275177,0.99475694,0.00004164331,0.0020593642,0.0017941312,0.00000985106],"about_ca_topic_score_codex":0.88267106,"about_ca_topic_score_gemma":0.6744054,"teacher_disagreement_score":0.11732894,"about_ca_system_score_codex":0.005317595,"about_ca_system_score_gemma":0.0059933686,"threshold_uncertainty_score":0.23603976},"labels":[],"label_agreement":null},{"id":"W2999368314","doi":"10.1029/2019jb018797","title":"Time‐Dependent Hydraulic Fracture Initiation","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Hydraulic Fracturing and Reservoir Analysis","field":"Engineering","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Schlumberger (Canada)","funders":"","keywords":"Hydraulic fracturing; Poromechanics; Brittleness; Geotechnical engineering; Geology; Fluid dynamics; Fracture (geology); Viscosity; Dissipation; Flow (mathematics); Mechanics; Materials science; Composite material; Porous medium; Porosity; Thermodynamics","score_opus":0.02520861189142049,"score_gpt":0.29810606414572294,"score_spread":0.27289745225430245,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2999368314","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9588803,0.00016446854,0.038150102,0.000019383704,0.000007707401,0.0000215189,0.0001543796,0.00018931947,0.0024128326],"genre_scores_gemma":[0.9984113,0.000034831373,0.0010524401,0.0000016618227,5.807812e-7,0.000007561812,0.000047357025,0.000005283529,0.00043889513],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999895,0.000006890002,0.0000044992366,0.000024736366,0.000048365404,0.000020510903],"domain_scores_gemma":[0.9997229,0.00010501872,0.000059287446,0.000043387456,0.00005379815,0.000015694843],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000179236,0.0002053207,0.0001580748,0.00035511365,0.00011909771,0.00017031029,0.00043577448,0.0002505809,0.00086773786],"category_scores_gemma":[0.00061022723,0.00015685009,0.00022878266,0.0001632949,0.0002469311,0.0002942673,0.00017933789,0.00030221065,0.00015444301],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020787856,0.00010234732,0.014288434,0.00010632801,0.000022759765,0.0002774634,0.0001462356,0.44252554,0.5085576,0.0026073204,0.00021107185,0.030946987],"study_design_scores_gemma":[0.0000042525594,0.00009203931,0.009424487,0.000006512987,0.0000059567933,0.00009050682,0.000023603498,0.8363078,0.15325935,0.00036349692,0.0004018678,0.000020136033],"about_ca_topic_score_codex":0.0022093179,"about_ca_topic_score_gemma":0.0020227626,"teacher_disagreement_score":0.0022093179,"about_ca_system_score_codex":0.00047185217,"about_ca_system_score_gemma":0.00027663592,"threshold_uncertainty_score":0.004392922},"labels":[],"label_agreement":null},{"id":"W3000153556","doi":"10.1029/2022jb024704","title":"Investigating the Effect of Mantle Flow and Viscosity Structure on Surface Velocities in Alaska Using 3‐D Geodynamic Models","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Aeronautics and Space Administration; National Science Foundation","keywords":"Geology; Plate tectonics; Subduction; Mantle (geology); Slab; Seismology; North American Plate; Tectonics; Geodesy; Geodynamics; Ocean surface topography; Lithosphere; Geophysics","score_opus":0.036832949049705216,"score_gpt":0.3026939215059327,"score_spread":0.26586097245622753,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3000153556","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99090356,0.00006687444,0.0069278404,0.00007686827,0.000009666498,0.000009611838,0.00026299644,0.0001442013,0.0015982992],"genre_scores_gemma":[0.99783945,0.0000538298,0.0016709873,0.00000735704,0.0000020724763,0.000008544936,0.00012315749,0.000008278419,0.00028626894],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999378,0.00001532337,0.0000061983146,0.00001719555,0.000013514653,0.00001004613],"domain_scores_gemma":[0.9996766,0.00017315758,0.000047658767,0.000029287326,0.00004640639,0.00002697941],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028278015,0.0004150807,0.00025796657,0.00048053538,0.0004888123,0.00077886716,0.00042874145,0.00085528265,0.00087541225],"category_scores_gemma":[0.0011512822,0.0005037102,0.0006353153,0.00030870104,0.00041427842,0.0005600415,0.00044363207,0.000431505,0.00013594194],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003220621,0.000031535103,0.015161186,0.00000934187,0.00002335618,0.000038102276,0.00004947527,0.9807342,0.0018784115,0.00032219623,0.000047230846,0.0016726778],"study_design_scores_gemma":[0.000007482952,0.000016591319,0.0065265265,0.00000485638,0.000011166761,0.0000074786713,0.000024900392,0.99243563,0.000650712,0.0001747642,0.00012938319,0.000010348715],"about_ca_topic_score_codex":0.10713088,"about_ca_topic_score_gemma":0.051674563,"teacher_disagreement_score":0.10713088,"about_ca_system_score_codex":0.00093768706,"about_ca_system_score_gemma":0.00078841345,"threshold_uncertainty_score":0.2130146},"labels":[],"label_agreement":null},{"id":"W3000496716","doi":"10.1029/2019jb018582","title":"Shear Velocity Model of Alaska Via Joint Inversion of Rayleigh Wave Ellipticity, Phase Velocities, and Receiver Functions Across the Alaska Transportable Array","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":74,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Terrane; Seismology; Asthenosphere; Crust; Volcano; North American Plate; Basin and range topography; Mantle (geology); Geophysics; Geomorphology; Tectonics; Lithosphere; Plate tectonics","score_opus":0.07711832854481288,"score_gpt":0.30015474910156886,"score_spread":0.223036420556756,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3000496716","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96083045,0.000065815206,0.03546297,0.00014001694,0.000018182085,0.000010890473,0.0005393037,0.00025911536,0.0026732462],"genre_scores_gemma":[0.99515176,0.00002358621,0.0039556716,0.000008052524,0.0000033571314,0.000007309783,0.00020703112,0.000008292577,0.00063506834],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99994075,0.000012152238,0.0000040812956,0.000021987535,0.000012371326,0.0000086901155],"domain_scores_gemma":[0.99984777,0.000049097842,0.00003382939,0.000014596578,0.000037939943,0.00001671069],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016146371,0.00031207863,0.00021318858,0.00027314917,0.0003451504,0.00050664414,0.00060265907,0.00047706717,0.0010385574],"category_scores_gemma":[0.0005421413,0.0003370508,0.0003967431,0.00035715717,0.00040267062,0.00037132826,0.0003274216,0.00041520514,0.00012870792],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016496837,0.0000081419685,0.0060002063,0.0000027389967,0.000012996382,0.0000357684,0.000016420665,0.99174845,0.00057303807,0.00034184917,0.000051889783,0.0011920034],"study_design_scores_gemma":[0.00000641424,0.0000094730985,0.0018526178,0.000001675121,0.0000068911095,0.0000067488068,0.0000128378115,0.9974915,0.00020426651,0.00030185236,0.000100309386,0.0000054296233],"about_ca_topic_score_codex":0.13085471,"about_ca_topic_score_gemma":0.09016012,"teacher_disagreement_score":0.13085471,"about_ca_system_score_codex":0.00070523424,"about_ca_system_score_gemma":0.0011734315,"threshold_uncertainty_score":0.26018614},"labels":[],"label_agreement":null},{"id":"W3002343616","doi":"10.1029/2019jb018432","title":"Azimuthal Anisotropy of the North American Upper Mantle Based on Full Waveform Inversion","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Subduction; Azimuth; Seismology; Mantle (geology); Seismogram; Amplitude; Slab; Anisotropy; Crust; Perpendicular; Inversion (geology); Geophysics; Geodesy; Tectonics; Geometry; Physics","score_opus":0.03177314488601523,"score_gpt":0.2815762958957222,"score_spread":0.24980315100970696,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3002343616","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.78737193,0.00017342123,0.19915687,0.00022545061,0.000025703317,0.000028929293,0.0010983872,0.00081816304,0.011101113],"genre_scores_gemma":[0.98582494,0.00008647578,0.012221474,0.000017340142,0.000007135116,0.00002157135,0.00062236737,0.00004516509,0.0011535527],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999448,0.000012449823,0.0000031179547,0.000013814436,0.000015088989,0.0000106985735],"domain_scores_gemma":[0.99991703,0.000016430802,0.00001470846,0.000014713736,0.00002733193,0.000009915976],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013792819,0.00040291925,0.000232953,0.00041316837,0.00019467685,0.00068047136,0.0006550805,0.00032299306,0.0012519147],"category_scores_gemma":[0.00043846545,0.00030502945,0.00039125903,0.00037671905,0.00019402288,0.000543488,0.00031549344,0.00036634918,0.00029664751],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000035961868,0.000024431749,0.0059217326,0.000010555632,0.000037967115,0.00006665718,0.0000249392,0.96679974,0.0068927114,0.001959583,0.00043051413,0.01779528],"study_design_scores_gemma":[0.0000034341308,0.0000024088272,0.0014036685,9.726325e-7,0.0000039597194,0.00000682163,0.000004926,0.9977884,0.0002479272,0.00032181243,0.00021205042,0.0000035624712],"about_ca_topic_score_codex":0.04581419,"about_ca_topic_score_gemma":0.031075861,"teacher_disagreement_score":0.04581419,"about_ca_system_score_codex":0.00034189556,"about_ca_system_score_gemma":0.0009538312,"threshold_uncertainty_score":0.09109503},"labels":[],"label_agreement":null},{"id":"W3002352831","doi":"10.1029/2019jb018310","title":"Shear Velocity and Radial Anisotropy beneath Southwestern Canada: Evidence for Crustal Extension and Thick‐Skinned Tectonics","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Eva Crane Trust","keywords":"Geology; Craton; Foreland basin; Seismology; Crust; Allochthon; Shear zone; Tectonics; Shear (geology); Thrust fault; Paleontology; Nappe","score_opus":0.08972848156065577,"score_gpt":0.32403381421892463,"score_spread":0.23430533265826886,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3002352831","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997077,0.00017410252,0.00006241154,0.00006990307,0.0000018456761,0.0000047774042,0.0006816643,0.000011039365,0.0019172614],"genre_scores_gemma":[0.999132,0.00010915836,0.000095316,0.000010720647,0.0000012912941,0.0000013033048,0.00025380251,0.0000017412823,0.0003946818],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998692,0.0000039171173,0.0000058023898,0.000028869092,0.000040015377,0.000052135223],"domain_scores_gemma":[0.99940753,0.000035613426,0.00009191654,0.000024046514,0.0003354007,0.0001054524],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012364368,0.00024383632,0.00016000879,0.0013292112,0.0010967901,0.0008296544,0.00034079142,0.00019978418,0.0022722883],"category_scores_gemma":[0.000667777,0.0001675829,0.00011872059,0.0016975397,0.00063007645,0.00016663354,0.0004486221,0.00019347144,0.00015123967],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008147073,0.000012177883,0.97693413,0.000024920831,0.000030337402,0.00019346965,0.00071037206,0.0003512846,0.008748474,0.00017441061,0.00036375728,0.012375245],"study_design_scores_gemma":[0.000001890686,0.0000020122468,0.9991449,0.00000604772,0.0000044328594,0.000022613782,0.0002536543,0.0001863347,0.00014231457,0.000014118398,0.0002187056,0.0000029096198],"about_ca_topic_score_codex":0.9731663,"about_ca_topic_score_gemma":0.9891802,"teacher_disagreement_score":0.026833713,"about_ca_system_score_codex":0.004671457,"about_ca_system_score_gemma":0.0057290215,"threshold_uncertainty_score":0.05398345},"labels":[],"label_agreement":null},{"id":"W3004929911","doi":"10.1029/2019jb018247","title":"Three‐Dimensional Mapping of Mt. Ruapehu Volcano, New Zealand, From Aeromagnetic Data Inversion and Hyperspectral Imaging","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Sill; Volcano; Inversion (geology); Dike; Hyperspectral imaging; Magnetic anomaly; Lava; Ridge; Seismology; Petrology; Geophysics; Mineralogy; Remote sensing; Paleontology","score_opus":0.07961757981584801,"score_gpt":0.3144374794222347,"score_spread":0.23481989960638672,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3004929911","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9936139,0.0000830455,0.0023907905,0.0000903541,0.000006992542,0.000047915957,0.0009269376,0.00011310345,0.0027270452],"genre_scores_gemma":[0.99263895,0.00008551028,0.0054298337,0.000014304326,0.0000047726153,0.000022079674,0.00078410516,0.000021196041,0.0009993109],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999372,0.000002005775,0.000001915056,0.000018970539,0.000027509153,0.000012403722],"domain_scores_gemma":[0.9999106,0.000008922726,0.000020293284,0.00000722627,0.00003425,0.00001875897],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000110994086,0.00043770246,0.00017830837,0.00087328366,0.00029503982,0.0006486035,0.00028540037,0.0002679719,0.0009792653],"category_scores_gemma":[0.00033901032,0.00031523517,0.0003317663,0.00068990636,0.00031590127,0.00030898192,0.0003449479,0.00031401016,0.0001968178],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004231963,0.00019307017,0.22130102,0.0003202848,0.0002439372,0.0018216389,0.001919519,0.029513763,0.64728665,0.000498523,0.00262336,0.09385508],"study_design_scores_gemma":[0.000047963884,0.000033775235,0.9430875,0.000020554719,0.000057743197,0.00020631538,0.0004265642,0.046808235,0.0076217107,0.00007766834,0.0015738747,0.000038184637],"about_ca_topic_score_codex":0.3378934,"about_ca_topic_score_gemma":0.5026713,"teacher_disagreement_score":0.3378934,"about_ca_system_score_codex":0.0008470099,"about_ca_system_score_gemma":0.0010458322,"threshold_uncertainty_score":0.6718533},"labels":[],"label_agreement":null},{"id":"W3005438168","doi":"10.1029/2019jb018888","title":"Frictional Strengths of Subduction Thrust Rocks in the Region of Shallow Slow Earthquakes","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Japan Society for the Promotion of Science; European GNSS Agency; Natural Sciences and Engineering Research Council of Canada; National Stroke Foundation; McGill University","keywords":"Geology; Subduction; Basalt; Lithology; Seismology; Matrix (chemical analysis); Petrology; Tectonics; Materials science; Composite material","score_opus":0.06670261828134365,"score_gpt":0.31582380928264636,"score_spread":0.2491211910013027,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3005438168","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9998535,0.000018767329,0.000020865926,0.0000010877333,1.4978696e-7,6.644997e-7,0.00002581133,0.0000014313401,0.00007773006],"genre_scores_gemma":[0.9999335,0.000008286358,0.000012531014,3.482099e-7,2.3585567e-7,4.0667993e-7,0.000026801372,4.3226575e-7,0.000017564134],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993086,0.000006501174,0.000009043364,0.000022551016,0.000012261242,0.000018690671],"domain_scores_gemma":[0.9997788,0.000043957403,0.00008054589,0.000016899381,0.00003474492,0.000044920453],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012470271,0.00017559885,0.00023526185,0.0014607148,0.00018781533,0.00045640706,0.00014981712,0.0001856301,0.00055617845],"category_scores_gemma":[0.0005252503,0.00019203112,0.00013677565,0.0004569534,0.0002502292,0.00022873358,0.00029125033,0.00007819816,0.000097157455],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041492056,0.00004685511,0.7693328,0.00006255036,0.00012249967,0.0004922452,0.0005197953,0.004366684,0.21917823,0.00015389507,0.000059594393,0.0052498765],"study_design_scores_gemma":[0.0000029875468,0.000029724806,0.9945523,0.0000022016525,0.000012351594,0.00007279769,0.000104390914,0.001875303,0.003266067,0.000020230193,0.00005838903,0.0000033956585],"about_ca_topic_score_codex":0.0038255232,"about_ca_topic_score_gemma":0.0036269356,"teacher_disagreement_score":0.0038255232,"about_ca_system_score_codex":0.00028656842,"about_ca_system_score_gemma":0.000089764464,"threshold_uncertainty_score":0.0076065063},"labels":[],"label_agreement":null},{"id":"W3005560164","doi":"10.1029/2019jb018853","title":"Three dimensional Gravity Local Inversion Across the Area Struck by the 2016–2017 Seismic Events in Central Italy","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Density contrast; Inversion (geology); Seismology; Basement; Residual; Sequence (biology); Evaporite; Geophysics; Paleontology; Tectonics; Sedimentary rock","score_opus":0.04908998779821804,"score_gpt":0.3075318829168888,"score_spread":0.2584418951186708,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3005560164","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968227,0.00004420851,0.0010828226,0.000051667346,0.000008038639,0.0000045759425,0.0010388981,0.00018014904,0.00076693343],"genre_scores_gemma":[0.99771464,0.000020813308,0.0008987539,0.0000055644273,0.0000067814044,0.000003203003,0.0011767372,0.000012960922,0.0001605783],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999325,0.000008361455,0.0000044929006,0.000023524464,0.000010202782,0.000020745741],"domain_scores_gemma":[0.9998721,0.000024576915,0.000028745053,0.000020512896,0.00003440598,0.000019608482],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015045244,0.00036458034,0.0002226249,0.00089199364,0.00016862091,0.0004293351,0.00040692673,0.00031035033,0.0012047879],"category_scores_gemma":[0.0005238164,0.00020543308,0.0005065316,0.00085328025,0.00022843131,0.00019181409,0.00036931562,0.0002289101,0.00029544174],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00075015606,0.0002911303,0.41464278,0.000131329,0.0002990487,0.00069518207,0.00045014793,0.50501454,0.022405347,0.00084057736,0.0022342694,0.052245475],"study_design_scores_gemma":[0.00007378583,0.00006238588,0.49851775,0.000017344879,0.000059985447,0.00009359265,0.00021758102,0.497648,0.001860378,0.00023253229,0.0011854402,0.00003126655],"about_ca_topic_score_codex":0.07362639,"about_ca_topic_score_gemma":0.080100276,"teacher_disagreement_score":0.07362639,"about_ca_system_score_codex":0.00051634636,"about_ca_system_score_gemma":0.0007645167,"threshold_uncertainty_score":0.14639568},"labels":[],"label_agreement":null},{"id":"W3007552588","doi":"10.1029/2019jb018248","title":"Constraining Interseismic Deformation of the Cascadia Subduction Zone: New Insights From Estimates of Vertical Land Motion Over Different Timescales","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada; Government of Ontario; University of Ottawa","keywords":"Geology; Subduction; Seismology; Residual; Holocene; Geodesy; Post-glacial rebound; Inversion (geology); Bathymetry; Sea level; Tectonics; Paleontology; Oceanography","score_opus":0.040239304672424155,"score_gpt":0.29277772318472406,"score_spread":0.2525384185122999,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3007552588","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9947366,0.00017748575,0.003556792,0.000045855224,0.0000024358649,0.0000033115502,0.00039856354,0.000058498452,0.0010204375],"genre_scores_gemma":[0.9990694,0.000049516457,0.0005778181,0.0000027220808,0.0000015615518,0.0000015104266,0.00023205185,0.00000924959,0.00005615987],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984074,0.00003659838,0.000013622914,0.000069601694,0.000023183768,0.000016163947],"domain_scores_gemma":[0.9996018,0.00017684928,0.000063917054,0.00006788055,0.000049926795,0.000039692186],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005871704,0.0004358769,0.0002775135,0.0007782113,0.00021683682,0.0006945567,0.00032990135,0.00027121717,0.00082401163],"category_scores_gemma":[0.001901292,0.0003260952,0.0004234064,0.00080633024,0.00019864317,0.0004402364,0.0004470375,0.00032613528,0.0001481509],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012356954,0.000045328863,0.85978407,0.0000646674,0.0003412891,0.00006750658,0.00023376185,0.09823233,0.012637102,0.00038922785,0.00019764385,0.027883545],"study_design_scores_gemma":[0.0000130236,0.000043688196,0.8022443,0.000023434704,0.000087276494,0.00003584072,0.00022226256,0.19446841,0.0013812606,0.00049193256,0.00095863856,0.00002988855],"about_ca_topic_score_codex":0.035648007,"about_ca_topic_score_gemma":0.06127875,"teacher_disagreement_score":0.035648007,"about_ca_system_score_codex":0.0005071169,"about_ca_system_score_gemma":0.00044067367,"threshold_uncertainty_score":0.07088107},"labels":[],"label_agreement":null},{"id":"W3009364192","doi":"10.1029/2019jb018612","title":"Evolution of Elastic and Mechanical Properties During Fault Shear: The Roles of Clay Content, Fabric Development, and Porosity","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"Geothermal Technologies Office; National Science Foundation","keywords":"Porosity; Clay minerals; Shearing (physics); Geology; Shear (geology); Stiffness; Elastic modulus; Composite material; Geotechnical engineering; Mineralogy; Materials science","score_opus":0.07818661726346422,"score_gpt":0.27580483862718297,"score_spread":0.19761822136371876,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3009364192","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99975413,0.0000205465,0.00007568471,0.0000038500575,3.7344967e-7,9.707085e-7,0.000049142523,0.0000027702433,0.00009262796],"genre_scores_gemma":[0.99981564,0.000009986561,0.00005248347,0.000002187297,1.7449456e-7,0.0000010895349,0.00003774554,0.0000017273035,0.00007901253],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999201,0.000009306472,0.000007634909,0.000020909669,0.000020396565,0.000021580408],"domain_scores_gemma":[0.9997259,0.000052452237,0.000096747885,0.000023221264,0.000056636018,0.000045000485],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017881472,0.00020477206,0.0001849261,0.0003151868,0.0001790061,0.0004842588,0.00014095579,0.00021234245,0.0008262584],"category_scores_gemma":[0.00037104252,0.00018589046,0.00011680768,0.00024535193,0.00041121512,0.00025820994,0.0002352522,0.00029422072,0.00010609843],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018808468,0.000028850296,0.033475608,0.000023339273,0.000016218544,0.00007437521,0.00008156266,0.0012143805,0.9633703,0.000050805513,0.000020620617,0.0014557363],"study_design_scores_gemma":[0.000010601886,0.00025937194,0.6033706,0.000008338945,0.00002109589,0.00012505,0.0004580198,0.012006095,0.38325182,0.000105306375,0.00036285393,0.000020740625],"about_ca_topic_score_codex":0.0023343917,"about_ca_topic_score_gemma":0.0027965447,"teacher_disagreement_score":0.0023343917,"about_ca_system_score_codex":0.00030738444,"about_ca_system_score_gemma":0.00012262721,"threshold_uncertainty_score":0.004641652},"labels":[],"label_agreement":null},{"id":"W3010488991","doi":"10.1029/2019jb019101","title":"Coupled Evolution of Deformation, Pore Fluid Pressure, and Fluid Flow in Shallow Subduction Forearcs","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"United States Science Support Program; Marsden Fund; Center for Hierarchical Manufacturing, National Science Foundation","keywords":"Geology; Subduction; Pore water pressure; Forearc; Fluid dynamics; Geotechnical engineering; Permeability (electromagnetism); Petrology; Tectonics; Seismology; Mechanics","score_opus":0.03688458353640006,"score_gpt":0.28625784872993937,"score_spread":0.2493732651935393,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3010488991","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992015,0.00001283425,0.0005878776,0.000012162075,4.8228304e-7,0.0000014453066,0.00003061394,0.000025289846,0.00012797932],"genre_scores_gemma":[0.9996275,0.000009367699,0.00024158301,0.0000030357958,5.039944e-7,0.0000019420756,0.000037560418,0.0000033643153,0.000075149466],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99994195,0.000009275679,0.00000499149,0.000016067675,0.000011689651,0.00001606881],"domain_scores_gemma":[0.99985826,0.000039843355,0.000040829702,0.000017397677,0.000021554228,0.00002199134],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012624926,0.00026242915,0.0002977046,0.0004569837,0.00023322146,0.00047617874,0.00044134274,0.000708989,0.0006542575],"category_scores_gemma":[0.00054397574,0.00037992836,0.00045490463,0.00028899248,0.0005324706,0.00030795851,0.00041199377,0.00028064303,0.000080312006],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002541712,0.00023457235,0.124932654,0.000048910784,0.00014463897,0.00062930846,0.0003089282,0.7363522,0.12881024,0.0012632617,0.00012397184,0.0068971487],"study_design_scores_gemma":[0.000033919318,0.00011727675,0.11403115,0.000007305553,0.000025832278,0.00009446622,0.000102029204,0.87876886,0.0061664046,0.00049071125,0.00013571983,0.000026361198],"about_ca_topic_score_codex":0.010953454,"about_ca_topic_score_gemma":0.006403433,"teacher_disagreement_score":0.010953454,"about_ca_system_score_codex":0.00085459807,"about_ca_system_score_gemma":0.000438796,"threshold_uncertainty_score":0.021779418},"labels":[],"label_agreement":null},{"id":"W3013767667","doi":"10.1029/2019jb018519","title":"Seismic <i>P</i>  Wave Velocity Model From 3‐D Surface and Borehole Seismic Data at the Alpine Fault DFDP‐2 Drill Site (Whataroa, New Zealand)","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta; Penn West Exploration (Canada); University of Calgary","funders":"","keywords":"Geology; Seismology; Borehole; Vertical seismic profile; Seismic velocity; Fault (geology); Drill hole; Basement; Surface wave; Geophysical imaging; Seismic tomography; Geodesy; Geophysics; Drill; Paleontology","score_opus":0.09256110426533741,"score_gpt":0.3089365733585767,"score_spread":0.2163754690932393,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3013767667","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99038637,0.000029678224,0.005825982,0.00008786124,0.00000969884,0.00003220954,0.0016842451,0.00035960675,0.0015843526],"genre_scores_gemma":[0.99581015,0.000030359224,0.0025405097,0.000008398698,0.0000033309345,0.000017638364,0.0013048508,0.000030005842,0.00025477447],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99993026,0.0000067368364,0.0000042815323,0.000020937017,0.000019434061,0.000018286217],"domain_scores_gemma":[0.99986684,0.000027086544,0.000031064206,0.000016531118,0.000037807822,0.000020674383],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015124386,0.00048317848,0.00021444891,0.0004752292,0.0002657107,0.0006622962,0.00071879313,0.00066880597,0.0008776079],"category_scores_gemma":[0.00067126856,0.00034025006,0.00052445434,0.0004740574,0.00030249084,0.0003770801,0.00021614203,0.00044387125,0.00029480897],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002734793,0.00014576675,0.12245734,0.000059865357,0.00008193509,0.00065082376,0.00030731977,0.83516884,0.0185789,0.0005392365,0.0018788527,0.019857703],"study_design_scores_gemma":[0.00007440297,0.000054735043,0.12535852,0.000013678072,0.000019923431,0.00009691879,0.00009097586,0.8721158,0.0013448574,0.00020433428,0.00057759706,0.00004829084],"about_ca_topic_score_codex":0.2207872,"about_ca_topic_score_gemma":0.1475253,"teacher_disagreement_score":0.2207872,"about_ca_system_score_codex":0.0011684969,"about_ca_system_score_gemma":0.0009767895,"threshold_uncertainty_score":0.43900412},"labels":[],"label_agreement":null},{"id":"W3016532136","doi":"10.1029/2020jb019731","title":"3‐D Magnetotelluric Imaging of the Easternmost Kunlun Fault: Insights Into Strain Partitioning and the Seismotectonics of the Jiuzhaigou Ms7.0 Earthquake","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"China Scholarship Council; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Magnetotellurics; Geology; Crust; Electrical resistivity and conductivity; Seismology; Fault (geology); Seismotectonics; Petrology; Mantle (geology); Upper crust; Geophysics","score_opus":0.027932295559811592,"score_gpt":0.28691098455158537,"score_spread":0.2589786889917738,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3016532136","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980989,0.000056232704,0.0010551421,0.000055144326,0.0000028007507,0.0000031794284,0.00016990151,0.00005780564,0.0005008022],"genre_scores_gemma":[0.99927074,0.00002450418,0.0004910419,0.000007340801,0.000002371126,0.000001763803,0.00010440165,0.000004663072,0.0000931149],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997354,0.000003544858,0.0000013821731,0.000007485451,0.0000051678708,0.000008910276],"domain_scores_gemma":[0.9999565,0.0000063046514,0.000011196581,0.000004717177,0.000008634144,0.000012670231],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000074152784,0.000266531,0.00021403526,0.00060493394,0.00020810997,0.0005243824,0.00021713701,0.0003429289,0.00059281586],"category_scores_gemma":[0.00016668456,0.00022558664,0.0002770783,0.00043425118,0.00020721738,0.00022984747,0.00026228683,0.00015206478,0.00009766752],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00053262064,0.00025057784,0.4893878,0.00011945232,0.00022223903,0.0015074426,0.0010192797,0.21051599,0.2554552,0.0014534062,0.0013984384,0.038137637],"study_design_scores_gemma":[0.000033498425,0.000052332012,0.61262786,0.000014733636,0.0000491407,0.00016791114,0.00040016236,0.3812824,0.0042564394,0.00040573455,0.0006547602,0.000055079814],"about_ca_topic_score_codex":0.014465312,"about_ca_topic_score_gemma":0.022553265,"teacher_disagreement_score":0.014465312,"about_ca_system_score_codex":0.00031002442,"about_ca_system_score_gemma":0.00025958408,"threshold_uncertainty_score":0.028762221},"labels":[],"label_agreement":null},{"id":"W3016706320","doi":"10.1029/2019jb019111","title":"An Absolute Paleogeographic Positioning of the Early Permian Tarim Large Igneous Province","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Norges Forskningsråd","keywords":"Permian; Geology; Paleomagnetism; Paleontology; Mantle plume; Mantle (geology); Carboniferous; Shear zone; Early Triassic; Longitude; Igneous rock; Geophysics; Latitude; Geodesy; Tectonics; Lithosphere","score_opus":0.024983180813225522,"score_gpt":0.27539779655801283,"score_spread":0.2504146157447873,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3016706320","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99822706,0.000064978965,0.0003658621,0.000009168542,0.0000015136358,0.000003084638,0.00010882542,0.000008923789,0.0012105507],"genre_scores_gemma":[0.9993599,0.000019558855,0.00036130866,0.0000014152532,0.0000012707595,0.0000016733521,0.00015398233,0.0000027465949,0.00009812489],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999329,0.000006927873,0.0000041747626,0.000025473819,0.00001353254,0.000016911788],"domain_scores_gemma":[0.9999355,0.0000081418575,0.000019324016,0.000008419203,0.000021880132,0.0000066718735],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015283449,0.0001344922,0.00012587805,0.0010348724,0.00025029056,0.00034993901,0.00018577812,0.000112621754,0.0010912238],"category_scores_gemma":[0.0002530654,0.00010348962,0.00015390952,0.00077549263,0.00017243045,0.00012830747,0.0003261418,0.00012681392,0.00021165962],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021966649,0.000029972938,0.902005,0.00006282733,0.00007162457,0.00028708222,0.00086325686,0.0028364416,0.044568084,0.000805516,0.00016299167,0.048087522],"study_design_scores_gemma":[0.000006709817,0.00002539068,0.99398696,0.000009828988,0.00001793694,0.00017472,0.00029500216,0.0022867902,0.0022285758,0.000056900502,0.00090745086,0.000003662304],"about_ca_topic_score_codex":0.008453186,"about_ca_topic_score_gemma":0.019767795,"teacher_disagreement_score":0.008453186,"about_ca_system_score_codex":0.00026911637,"about_ca_system_score_gemma":0.00040229456,"threshold_uncertainty_score":0.016807973},"labels":[],"label_agreement":null},{"id":"W3017010532","doi":"10.1029/2020jb019388","title":"Damage Evolution During Rock Pulverization Induced by Dynamic Compressive Loading","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Rock Mechanics and Modeling","field":"Engineering","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Science Foundation of Tianjin City; National Natural Science Foundation of China","keywords":"Split-Hopkinson pressure bar; Dynamic loading; Compression (physics); Dynamic range compression; Geology; Strain rate; Shear (geology); Geotechnical engineering; Dynamic load testing; Fault (geology); Strain (injury); Bar (unit); Materials science; Fracture (geology); Composite material; Seismology","score_opus":0.027274959413574197,"score_gpt":0.2966696148952282,"score_spread":0.269394655481654,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3017010532","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995184,0.000054079293,0.00022328665,0.000003790678,0.0000011948949,0.0000035665555,0.000031719323,0.000013904111,0.00015015826],"genre_scores_gemma":[0.99969125,0.000021437681,0.00010970896,0.0000032136302,6.28988e-7,0.000002559326,0.00003489276,0.0000020576533,0.0001342892],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989426,0.0000089712485,0.000005731106,0.000020233263,0.000040987503,0.00002977156],"domain_scores_gemma":[0.999747,0.00005317571,0.00007503656,0.000036428366,0.00005244974,0.000035838228],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000113934715,0.00019033473,0.00017907389,0.00040316512,0.00017890015,0.00015198461,0.00020165896,0.00020784701,0.0010330146],"category_scores_gemma":[0.0002554649,0.00012151003,0.00009191357,0.00022362928,0.0003584546,0.0001840736,0.00018591828,0.00018012672,0.00006534246],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030636997,0.000036713995,0.0067452877,0.00003527247,0.000011786607,0.0003058588,0.00013029196,0.0027606783,0.9838013,0.00003463328,0.00004531533,0.0057864203],"study_design_scores_gemma":[0.000014480378,0.00081512507,0.21040104,0.000008854041,0.000022115997,0.0003677941,0.00022453468,0.022694886,0.76485074,0.00005668989,0.00052523543,0.000018543908],"about_ca_topic_score_codex":0.0016923395,"about_ca_topic_score_gemma":0.0028184808,"teacher_disagreement_score":0.0016923395,"about_ca_system_score_codex":0.00025985003,"about_ca_system_score_gemma":0.000089601126,"threshold_uncertainty_score":0.003455758},"labels":[],"label_agreement":null},{"id":"W3019336886","doi":"10.1029/2020jb020354","title":"Creep Burst Coincident With Faulting in Marble Observed in 4‐D Synchrotron X‐Ray Imaging Triaxial Compression Experiments","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Environmental Studies Research Funds; Norges Forskningsråd; European Synchrotron Radiation Facility","keywords":"Creep; Geology; Slip (aerodynamics); Shearing (physics); Strain rate; Nucleation; Deformation (meteorology); Materials science; Mineralogy; Geotechnical engineering; Composite material; Thermodynamics","score_opus":0.09272857214629587,"score_gpt":0.34162070210050166,"score_spread":0.2488921299542058,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3019336886","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992601,0.00004704167,0.00034927193,0.000010463144,0.0000015858692,0.0000050973067,0.00006401988,0.00001867646,0.00024366326],"genre_scores_gemma":[0.99884737,0.000042051608,0.0005210786,0.000007799208,0.0000020875434,0.000009774667,0.00014349201,0.000008045438,0.0004182464],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999045,0.0000072551384,0.0000070564215,0.000018611916,0.00003740776,0.000025135756],"domain_scores_gemma":[0.99952507,0.00007055268,0.00015798719,0.00006477823,0.00009891075,0.00008274996],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013198823,0.00022755614,0.0001627437,0.00047263768,0.00023408336,0.00033028872,0.00031256455,0.00035539203,0.0009816011],"category_scores_gemma":[0.0003274157,0.00022266059,0.00015222552,0.00036091523,0.00028485287,0.00018024407,0.00021574032,0.00031434774,0.00012994927],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010911856,0.000035290257,0.0067569804,0.00001541307,0.000007906143,0.00018158324,0.00009496672,0.00036398912,0.9910188,0.00003210574,0.000023386487,0.001360525],"study_design_scores_gemma":[0.000018210087,0.0003483782,0.35984305,0.000008909851,0.000017978136,0.0004415345,0.0001889798,0.008033115,0.6302443,0.00004649403,0.0007901664,0.000018919862],"about_ca_topic_score_codex":0.002720816,"about_ca_topic_score_gemma":0.00527518,"teacher_disagreement_score":0.002720816,"about_ca_system_score_codex":0.00045118312,"about_ca_system_score_gemma":0.00013709084,"threshold_uncertainty_score":0.0054100156},"labels":[],"label_agreement":null},{"id":"W3022070826","doi":"10.1029/2019jb018734","title":"Lateral Variations in Thermochemical Structure of the Eastern Canadian Shield","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Ministério da Educação; Coordenação de Aperfeiçoamento de Pessoal de Nível Superior; Natural Environment Research Council; Sight Research UK","keywords":"Geology; Lithosphere; Craton; Archean; Precambrian; Xenolith; Subduction; Crust; Shield; Metasomatism; Proterozoic; Geophysics; Baltic Shield; Petrology; Geochemistry; Seismology; Mantle (geology); Tectonics","score_opus":0.030998173444198026,"score_gpt":0.26646108870899604,"score_spread":0.235462915264798,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3022070826","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99693847,0.00006458189,0.00009147503,0.000029427481,0.0000014495989,0.0000040063087,0.00079172937,0.000015460677,0.002063414],"genre_scores_gemma":[0.9991372,0.000030766972,0.00011578216,0.000005409454,3.4761658e-7,0.0000013673433,0.00038133544,0.0000031354068,0.0003245117],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990296,0.0000037112256,0.0000028567197,0.000027891458,0.000027930826,0.00003468236],"domain_scores_gemma":[0.99980074,0.000014099588,0.000024838371,0.000009378835,0.00011398812,0.000037089234],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000097968805,0.00023219726,0.0001602757,0.0010798014,0.0010001141,0.000834308,0.00047400835,0.00023412355,0.00180716],"category_scores_gemma":[0.00036454923,0.00017145036,0.00026565194,0.00089197967,0.00046592005,0.00016681828,0.00037837808,0.0001407233,0.00015871806],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012958705,0.000020303716,0.9505609,0.00003949654,0.0001121843,0.0001791907,0.0007108272,0.018072672,0.01619894,0.001047778,0.00084369,0.012084431],"study_design_scores_gemma":[0.000004549213,0.000004743299,0.9910793,0.000008527156,0.000011606225,0.000029273173,0.00034976614,0.006740845,0.00050250185,0.00007022972,0.0011840122,0.000014635142],"about_ca_topic_score_codex":0.9784097,"about_ca_topic_score_gemma":0.990006,"teacher_disagreement_score":0.021590292,"about_ca_system_score_codex":0.010596193,"about_ca_system_score_gemma":0.0066227266,"threshold_uncertainty_score":0.07688117},"labels":[],"label_agreement":null},{"id":"W3025517681","doi":"10.1029/2019jb018453","title":"The Northern Terminus of Cascadia Subduction","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Geoscience BC; University of Victoria; University of Calgary; University of British Columbia","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Subduction; Geology; Seismology; Plate tectonics; Submarine pipeline; North American Plate; Lithosphere; Induced seismicity; Peninsula; Ridge; Triple junction; Oceanic crust; Convergent boundary; Tectonics; Paleontology; Oceanography","score_opus":0.05665269629307689,"score_gpt":0.3131148268378913,"score_spread":0.2564621305448144,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3025517681","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.983712,0.00013358578,0.00011934216,0.00014430792,0.000011956015,0.000007983434,0.000570982,0.00006262867,0.015237139],"genre_scores_gemma":[0.99793124,0.000058665002,0.00008604623,0.000010026898,0.0000037157383,0.0000034165043,0.00039509233,0.0000051555066,0.001506838],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994123,0.0000032522316,0.0000032657329,0.000022501537,0.000013997822,0.000015836898],"domain_scores_gemma":[0.999785,0.000011182135,0.000051536957,0.000015628068,0.00007732557,0.000059300743],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007333704,0.00024244103,0.00018042186,0.0006353677,0.0009736518,0.00044207854,0.00015716178,0.00018093699,0.0029850178],"category_scores_gemma":[0.00035339885,0.0001224823,0.00013502328,0.00055997877,0.00033256592,0.00011519869,0.00058764435,0.00019577266,0.0004083065],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028515706,0.000020816813,0.9513857,0.0001439933,0.00006913237,0.0017752564,0.0018938532,0.0031637314,0.018108636,0.0008903619,0.002357489,0.019905914],"study_design_scores_gemma":[0.0000046046907,0.0000098245655,0.99625045,0.000014986175,0.000008957004,0.00011292569,0.0004112918,0.000410143,0.00024193061,0.000083958235,0.002446845,0.000004164512],"about_ca_topic_score_codex":0.220154,"about_ca_topic_score_gemma":0.34698665,"teacher_disagreement_score":0.220154,"about_ca_system_score_codex":0.0015281818,"about_ca_system_score_gemma":0.0013771784,"threshold_uncertainty_score":0.4377451},"labels":[],"label_agreement":null},{"id":"W3028008725","doi":"10.1029/2020jb019933","title":"Reactivation of an Intraplate Fault by Mine‐Blasting Events: Implications to Regional Seismic Hazard in Western Canada","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Seismology; Induced seismicity; Geology; Intraplate earthquake; Seismic hazard; Trench; Fault (geology); Peak ground acceleration; Spectral acceleration; Seismic risk; Event (particle physics); Tectonics","score_opus":0.05613225326905229,"score_gpt":0.32066201325575566,"score_spread":0.26452975998670336,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3028008725","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964288,0.0001950492,0.00011611519,0.00015986849,0.0000029823334,0.00001123209,0.0009676894,0.000008420425,0.0021100068],"genre_scores_gemma":[0.9988984,0.00011663355,0.00008874426,0.000015036788,0.0000010605091,0.0000023123964,0.00028728665,0.000002240403,0.00058827514],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99975723,0.000015817728,0.000013732645,0.00004045575,0.000061267216,0.000111529254],"domain_scores_gemma":[0.99889576,0.00008002245,0.00017732385,0.000024683733,0.0005706904,0.0002515132],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020522182,0.00019804592,0.00022423925,0.0014737732,0.0015776302,0.0014117176,0.0005357152,0.00026397168,0.0015483319],"category_scores_gemma":[0.0011773973,0.00012185091,0.00017344355,0.0029040372,0.0006561442,0.00025436076,0.00063138996,0.00037071688,0.000121661324],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008502084,0.000025851248,0.981108,0.000038356593,0.000043226893,0.00036280972,0.0011070971,0.0015854329,0.0016824184,0.00032250074,0.00082156,0.01281775],"study_design_scores_gemma":[0.0000028669108,0.0000090559815,0.99395704,0.000021226555,0.000014126671,0.000058048136,0.0031093871,0.0016476354,0.00016369254,0.0000648721,0.00094362657,0.000008409846],"about_ca_topic_score_codex":0.99414295,"about_ca_topic_score_gemma":0.99778205,"teacher_disagreement_score":0.016508192,"about_ca_system_score_codex":0.016508192,"about_ca_system_score_gemma":0.017266922,"threshold_uncertainty_score":0.11977589},"labels":[],"label_agreement":null},{"id":"W3029970191","doi":"10.1029/2019jb019239","title":"<i>Vp</i>/<i>Vs</i> Ratio of Incoming Sediments Off Cascadia Subduction Zone From Analysis of Controlled‐Source Multicomponent OBS Records","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Science Foundation","keywords":"Geology; Accretionary wedge; Subduction; Submarine pipeline; Overpressure; Pore water pressure; Sedimentary rock; Sediment; Hydrostatic pressure; Seismology; Turbidite; Structural basin; Basement; Petrology; Geomorphology; Geochemistry; Tectonics; Oceanography; Geotechnical engineering","score_opus":0.043327755797265805,"score_gpt":0.3013103737667683,"score_spread":0.2579826179695025,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3029970191","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99876165,0.000019834111,0.000119520024,0.000003742083,6.6427685e-7,0.000002883952,0.0005154483,0.000025373249,0.0005509221],"genre_scores_gemma":[0.99846834,0.000027315662,0.00021526226,0.0000020744058,0.0000015923629,0.0000053694653,0.001111577,0.000012895968,0.00015570625],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998847,0.000006400502,0.000017377675,0.000040554627,0.00003330408,0.000017686381],"domain_scores_gemma":[0.9996567,0.000054496224,0.00010036523,0.000038818096,0.00009490497,0.000054772634],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015200373,0.00039680133,0.00015455161,0.00248903,0.00028521975,0.0005258003,0.00028358743,0.00024127973,0.0009999202],"category_scores_gemma":[0.0006751917,0.00024149443,0.0003313478,0.0015663853,0.00022611895,0.0002173081,0.00039455172,0.0001590632,0.00016971941],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013243867,0.000030494753,0.94944215,0.00005110794,0.00014936362,0.0002426215,0.00030995917,0.0025747048,0.035334628,0.000082562925,0.00019689993,0.011453042],"study_design_scores_gemma":[0.0000017860021,0.0000074696404,0.99848205,0.0000022480822,0.000014054187,0.000020817224,0.000056196,0.0006033481,0.00070459436,0.000006350693,0.00009876137,0.000002327554],"about_ca_topic_score_codex":0.033602502,"about_ca_topic_score_gemma":0.039916996,"teacher_disagreement_score":0.033602502,"about_ca_system_score_codex":0.0005803129,"about_ca_system_score_gemma":0.00024459773,"threshold_uncertainty_score":0.06681383},"labels":[],"label_agreement":null},{"id":"W3030099456","doi":"10.1029/2020jb020237","title":"A Mg Isotopic Perspective on the Mobility of Magnesium During Serpentinization and Carbonation of the Oman Ophiolite","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Division of Earth Sciences; Alfred P. Sloan Foundation; National Science Foundation","keywords":"Peridotite; Geology; Mantle (geology); Geochemistry; Ophiolite; Silicate; Olivine; Magnesite; Carbonate; Mineralogy; Metasomatism; Magnesium; Chemistry","score_opus":0.031131275614725645,"score_gpt":0.2765737708884136,"score_spread":0.24544249527368797,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3030099456","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983637,0.00012897488,0.000115186,0.00002340449,0.0000022549675,0.0000013893632,0.00014512394,0.000005948963,0.0012141152],"genre_scores_gemma":[0.99929345,0.00005413776,0.00012658635,0.000009854565,0.0000028932138,0.000001132692,0.00010591151,0.000004407537,0.00040159893],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99993193,0.0000046230684,0.0000041655353,0.000026141957,0.0000149983525,0.000018142886],"domain_scores_gemma":[0.9999523,0.0000058953274,0.000015047601,0.000003821058,0.000015833073,0.0000071401864],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009987839,0.00025098378,0.00010403461,0.0011948984,0.00043440086,0.0005414547,0.0002451555,0.00020648901,0.000973221],"category_scores_gemma":[0.0001334956,0.000101017846,0.000115428054,0.0005264181,0.0003304311,0.00029874837,0.00028765184,0.00014130473,0.00014136592],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00052711304,0.00002511698,0.34453917,0.000050292845,0.000062630585,0.00078049203,0.0008422776,0.0004839382,0.63434774,0.0005752737,0.00015948045,0.017606493],"study_design_scores_gemma":[0.0000052524138,0.00005264683,0.9653306,0.000007902799,0.00002258562,0.00026378524,0.0005416317,0.0009979043,0.029470539,0.0001743983,0.0031231355,0.000009591504],"about_ca_topic_score_codex":0.015000157,"about_ca_topic_score_gemma":0.023265895,"teacher_disagreement_score":0.015000157,"about_ca_system_score_codex":0.00080119405,"about_ca_system_score_gemma":0.00019588358,"threshold_uncertainty_score":0.029825687},"labels":[],"label_agreement":null},{"id":"W3032682931","doi":"10.1029/2019jb019184","title":"Crustal Structure of the Niuafo'ou Microplate and Fonualei Rift and Spreading Center in the Northeastern Lau Basin, Southwestern Pacific","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Bundesministerium für Bildung und Forschung","keywords":"Geology; Crust; Seafloor spreading; Island arc; Rift; Oceanic crust; Seismology; Underplating; Volcano; Accretion (finance); Volcanic arc; Subduction; Back-arc basin; Mantle (geology); Geophysics; Tectonics","score_opus":0.026189131076280372,"score_gpt":0.2701834881361935,"score_spread":0.2439943570599131,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3032682931","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992823,0.00007296221,0.000047345027,0.000007685638,5.0958226e-7,0.0000029480254,0.00006226711,0.0000055356772,0.0005185008],"genre_scores_gemma":[0.99965453,0.000037921545,0.00009908577,0.0000017138665,6.0667725e-7,0.0000028157888,0.0000872706,9.2837155e-7,0.00011512613],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999956,0.0000035331925,0.0000035478738,0.000014076262,0.000011098705,0.000011754384],"domain_scores_gemma":[0.9998816,0.000012189752,0.00004651761,0.0000071787495,0.00003221517,0.000020303405],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001126686,0.0002136002,0.0001525254,0.0012978023,0.0003924314,0.00041656857,0.00018181276,0.00017437067,0.00073922274],"category_scores_gemma":[0.00035602498,0.00016377549,0.00014214069,0.00070720114,0.00028651432,0.00023266043,0.0004363136,0.000100987505,0.00006483956],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004728294,0.000015179037,0.9766368,0.000034931618,0.0000426976,0.0002646477,0.0010830893,0.0010933401,0.010953402,0.00008104752,0.00008606631,0.009661481],"study_design_scores_gemma":[9.071707e-7,0.0000046834048,0.99906987,0.0000039660754,0.000004591212,0.000026922644,0.00015924031,0.0005132476,0.00011303336,0.000005724339,0.00009640836,0.0000014886817],"about_ca_topic_score_codex":0.10990486,"about_ca_topic_score_gemma":0.1599823,"teacher_disagreement_score":0.10990486,"about_ca_system_score_codex":0.00052734645,"about_ca_system_score_gemma":0.00038473395,"threshold_uncertainty_score":0.2185303},"labels":[],"label_agreement":null},{"id":"W3033582509","doi":"10.1029/2019jb019260","title":"Late Paleoproterozoic to Early Mesoproterozoic Mafic Magmatism in the SW Yangtze Block: Mantle Plumes Associated With Nuna Breakup?","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"Fundamental Research Funds for the Central Universities; Australian Research Council; Government Council on Grants, Russian Federation","keywords":"Mafic; Supercontinent; Geology; Geochemistry; Rodinia; Magmatism; Laurentia; Mantle plume; Craton; Petrology; Zircon; Mantle (geology); Lithosphere; Paleontology; Paleozoic; Tectonics","score_opus":0.03289917655727929,"score_gpt":0.26910989474587227,"score_spread":0.236210718188593,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3033582509","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99942905,0.000109500004,0.000031497617,0.000026270955,0.0000010008395,0.0000029469713,0.00007593978,0.000004490476,0.00031929486],"genre_scores_gemma":[0.99952483,0.0000647406,0.00006386674,0.0000059994927,0.0000018101866,0.000002972733,0.00011295485,0.0000015514798,0.0002212367],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996316,0.0000023624887,0.0000023902662,0.000010781488,0.000006212379,0.000015138488],"domain_scores_gemma":[0.99992716,0.0000060861244,0.0000267015,0.0000038549424,0.00001561143,0.000020578571],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011298091,0.00014379925,0.00015717241,0.0010913309,0.000416821,0.00040834353,0.00018577545,0.0001762544,0.0016356932],"category_scores_gemma":[0.00014570521,0.0001437492,0.00014308894,0.0008219343,0.00033439812,0.00033339887,0.0004976464,0.00013104317,0.00010135662],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011753494,0.000016574822,0.9575403,0.000047587284,0.000036784142,0.0004862112,0.0018812632,0.00013089995,0.031581376,0.00019998764,0.00007661774,0.00788495],"study_design_scores_gemma":[0.0000023069092,0.000009000315,0.99849916,0.0000036617007,0.000007196937,0.00006339235,0.000565795,0.00014420117,0.00038604144,0.000028403967,0.0002882842,0.0000025762101],"about_ca_topic_score_codex":0.03735772,"about_ca_topic_score_gemma":0.08426596,"teacher_disagreement_score":0.03735772,"about_ca_system_score_codex":0.00060500624,"about_ca_system_score_gemma":0.00043597555,"threshold_uncertainty_score":0.07428056},"labels":[],"label_agreement":null},{"id":"W3035681603","doi":"10.1029/2019jb019095","title":"Are Aftershock Sequences Pertinent to Long‐Term Seismic Hazard Assessments? Insights From the Temporal ETAS Model","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Aftershock; Induced seismicity; Seismology; Magnitude (astronomy); Geology; Poisson distribution; Term (time); Hazard; Seismic hazard; Sequence (biology); Statistics; Mathematics; Physics","score_opus":0.11039703419095823,"score_gpt":0.354051205181799,"score_spread":0.24365417099084077,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3035681603","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7147816,0.0006133583,0.26789728,0.0027974576,0.00008078498,0.00007326977,0.0010652528,0.0002645687,0.012426489],"genre_scores_gemma":[0.99366003,0.00022617284,0.0041796737,0.00005749052,0.00005050311,0.000024490044,0.00024028563,0.000025165955,0.0015362807],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9995813,0.00014087027,0.00003298322,0.00011309521,0.00007228181,0.000059367416],"domain_scores_gemma":[0.9933269,0.0038564764,0.0016364177,0.00031517862,0.0005650364,0.00030002964],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0027906226,0.00040993287,0.000479225,0.0010864037,0.00027812747,0.0016264266,0.0011068654,0.00083334104,0.002404647],"category_scores_gemma":[0.015476603,0.00030559386,0.00051319844,0.0010357975,0.0007925614,0.0024530722,0.00087415864,0.00075191405,0.00031311155],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001460829,0.00008429839,0.04359633,0.00007557231,0.00009179409,0.00025797103,0.00022236099,0.8550491,0.0017945232,0.08060927,0.0013884393,0.016684199],"study_design_scores_gemma":[0.000004623205,0.000011429891,0.003424613,0.000007630203,0.000009216745,0.000036934092,0.000056434543,0.9776642,0.000086484986,0.018430375,0.00025947264,0.000008675299],"about_ca_topic_score_codex":0.012282706,"about_ca_topic_score_gemma":0.0074730054,"teacher_disagreement_score":0.012282706,"about_ca_system_score_codex":0.0009463581,"about_ca_system_score_gemma":0.0009601013,"threshold_uncertainty_score":0.024422407},"labels":[],"label_agreement":null},{"id":"W3036514308","doi":"10.1029/2020jb020337","title":"Femtosecond X‐Ray Diffraction of Laser‐Shocked Forsterite (Mg<sub>2</sub>SiO<sub>4</sub>) to 122 GPa","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"SLAC National Accelerator Laboratory; Los Alamos National Laboratory; Lawrence Livermore National Laboratory; Office of Science; Office of the Dean for Research, Princeton University; National Science Foundation; Česká geologická služba; Laboratory Directed Research and Development; Fusion Energy Sciences; U.S. Department of Energy; Princeton University; Deutsche Forschungsgemeinschaft","keywords":"Forsterite; Crystallite; Materials science; Amorphous solid; Laser; Diffraction; Phase (matter); Femtosecond; Silicate perovskite; Crystal (programming language); Periclase; Analytical Chemistry (journal); Electron diffraction; Mineralogy; Crystallography; Optics; Perovskite (structure); Chemistry; Metallurgy; Physics","score_opus":0.036423137982934756,"score_gpt":0.29107846559259726,"score_spread":0.2546553276096625,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3036514308","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989184,0.000067662615,0.00017395294,0.000013965233,0.00000285148,0.0000025277582,0.00017455901,0.000021605594,0.0006244391],"genre_scores_gemma":[0.99845004,0.00006985302,0.00026255375,0.000008759222,0.0000027175254,0.000003962795,0.00032458492,0.000009863616,0.0008675655],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.999941,0.000002327907,0.0000023649045,0.000012188244,0.000028386825,0.000013777085],"domain_scores_gemma":[0.99990857,0.000019097293,0.0000253857,0.000007771591,0.000024218376,0.0000149960715],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000047403046,0.00017821435,0.00018102274,0.0002530128,0.000210142,0.0002107307,0.00021342553,0.00024647056,0.0018292668],"category_scores_gemma":[0.00012157526,0.0001427296,0.00011863617,0.00032298168,0.00018408851,0.00015213223,0.00013964833,0.00028856518,0.0001103215],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008945909,0.000010429767,0.0019123148,0.00002242887,0.000008506605,0.00010337146,0.00006274863,0.00025220454,0.99631387,0.00003179075,0.0000673285,0.001125587],"study_design_scores_gemma":[0.000024838942,0.00020558211,0.107512005,0.000007967796,0.00001434537,0.00020823053,0.00022780728,0.0031763692,0.8870509,0.000039566326,0.0015205668,0.000011785109],"about_ca_topic_score_codex":0.0031220512,"about_ca_topic_score_gemma":0.004320524,"teacher_disagreement_score":0.0031220512,"about_ca_system_score_codex":0.00034746007,"about_ca_system_score_gemma":0.00012605415,"threshold_uncertainty_score":0.006207764},"labels":[],"label_agreement":null},{"id":"W3037751930","doi":"10.1029/2020jb019714","title":"Optimization of the Match‐Filtering Method for Robust Repeating Earthquake Detection: The Multisegment Cross‐Correlation Approach","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismology and Earthquake Studies","field":"Computer Science","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Waveform; Computer science; Cross-correlation; Amplitude; Correlation; Filter (signal processing); Algorithm; Matched filter; Phase (matter); Reliability (semiconductor); Pattern recognition (psychology); Artificial intelligence; Physics; Mathematics; Statistics; Optics; Telecommunications; Computer vision","score_opus":0.08337811905209258,"score_gpt":0.35722042432650136,"score_spread":0.2738423052744088,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3037751930","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.02391725,0.00016394172,0.975089,0.000052797554,0.000014756428,0.000027637896,0.00003006246,0.0003187518,0.00038562273],"genre_scores_gemma":[0.3312943,0.00022223554,0.6665911,0.00009872512,0.000051377887,0.0001094404,0.00023637559,0.000144474,0.0012519965],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9992385,0.00016724104,0.000049704733,0.00018806841,0.00026846636,0.00008802366],"domain_scores_gemma":[0.9988293,0.0005306692,0.00016185454,0.00012320609,0.00029869392,0.00005625464],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015333651,0.00093391514,0.0009722317,0.001515479,0.00040276712,0.00063779886,0.000932071,0.00095953385,0.0013513622],"category_scores_gemma":[0.0033162693,0.00049580174,0.00081529294,0.0010570186,0.0004085226,0.0008877863,0.0008769542,0.00066139956,0.00038656188],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047025672,0.00028540537,0.004255009,0.00020165669,0.00025170957,0.00021245875,0.00012783676,0.40125293,0.09506093,0.008242046,0.0020975287,0.48754224],"study_design_scores_gemma":[0.000007965573,0.000054383076,0.0012010807,0.000005794243,0.000021711727,0.000040180148,0.0000084384,0.991319,0.0063226717,0.00051914254,0.00048656852,0.00001306737],"about_ca_topic_score_codex":0.0053321626,"about_ca_topic_score_gemma":0.004792685,"teacher_disagreement_score":0.0053321626,"about_ca_system_score_codex":0.00053506653,"about_ca_system_score_gemma":0.0015597964,"threshold_uncertainty_score":0.010602295},"labels":[],"label_agreement":null},{"id":"W3039720686","doi":"10.1029/2020jb019817","title":"Effects of Earthquake Recurrence on Localization of Interseismic Deformation Around Locked Strike‐Slip Faults","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Viscoelasticity; Seismology; Geodetic datum; Slip (aerodynamics); Deformation (meteorology); Fault (geology); Shear zone; Rheology; Geodesy; Materials science; Physics","score_opus":0.038905745073269236,"score_gpt":0.3025583879846737,"score_spread":0.2636526429114045,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3039720686","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999218,0.000045869496,0.00036171655,0.000012418204,0.0000016307542,0.000001168809,0.000030565465,0.00001592113,0.00031268215],"genre_scores_gemma":[0.9998733,0.000009991557,0.000028224507,0.000001962305,5.447731e-7,5.8615376e-7,0.000015541114,0.00000302366,0.000066729124],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998758,0.000047296904,0.00001008443,0.000025679909,0.0000144337255,0.000026625221],"domain_scores_gemma":[0.9980015,0.0011362268,0.0004465222,0.00013939042,0.00009981089,0.00017657103],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033961263,0.00025381084,0.00025173678,0.00031801776,0.00012369841,0.0004354701,0.00021918924,0.00027310857,0.0015833774],"category_scores_gemma":[0.0027417683,0.00012164799,0.00027604078,0.00019835019,0.00024235944,0.00029864383,0.00039530473,0.00018040554,0.00018798858],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0025399853,0.00042590353,0.48461667,0.00015483095,0.00034680802,0.0014102279,0.0003203378,0.37182936,0.11539544,0.00059997273,0.0003631454,0.021997314],"study_design_scores_gemma":[0.00006516416,0.0023804896,0.5793368,0.000034850338,0.00022487415,0.00038982483,0.00036740498,0.40242186,0.013958108,0.00045337903,0.00033333898,0.00003381401],"about_ca_topic_score_codex":0.0021287238,"about_ca_topic_score_gemma":0.0017475154,"teacher_disagreement_score":0.0021287238,"about_ca_system_score_codex":0.00020971146,"about_ca_system_score_gemma":0.00011118095,"threshold_uncertainty_score":0.005296886},"labels":[],"label_agreement":null},{"id":"W3040122085","doi":"10.1029/2020jb019430","title":"Depth‐Scanning Algorithm: Accurate, Automatic, and Efficient Determination of Focal Depths for Local and Regional Earthquakes","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Waveform; Geology; Algorithm; Phase (matter); Seismology; Focal mechanism; Tectonics; Constraint (computer-aided design); Computer science; Mathematics; Geometry; Physics; Telecommunications","score_opus":0.06468570908977624,"score_gpt":0.3342686452445277,"score_spread":0.2695829361547515,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3040122085","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.037640594,0.000085078434,0.9598378,0.000048365033,0.000018442472,0.00005890469,0.00009926302,0.0015552662,0.00065630104],"genre_scores_gemma":[0.15675509,0.00008480427,0.8421001,0.000026958493,0.000013029005,0.000067563,0.00020273976,0.000104969375,0.00064475194],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998148,0.000030028066,0.000013924041,0.000045080218,0.00007504808,0.000021049973],"domain_scores_gemma":[0.99960023,0.00010913009,0.000059863112,0.00005892075,0.00014523041,0.000026642057],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038617456,0.00060193316,0.000340485,0.0010524873,0.00024250137,0.00043822685,0.0007862441,0.00046914618,0.0016891089],"category_scores_gemma":[0.0015776256,0.00032493082,0.00024303718,0.0007708002,0.00021058448,0.0007100431,0.00058943377,0.00038412065,0.00071105413],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026173267,0.00007550642,0.0052935,0.00008594845,0.00003649407,0.000104444305,0.00014580543,0.039977234,0.17041437,0.0030997545,0.0027492214,0.7777559],"study_design_scores_gemma":[0.000073624746,0.00010677637,0.0056078364,0.000011691686,0.00002460876,0.00029548502,0.000062319064,0.92837626,0.05921815,0.0017739536,0.0044104587,0.000038906855],"about_ca_topic_score_codex":0.0025121933,"about_ca_topic_score_gemma":0.0040263925,"teacher_disagreement_score":0.0025121933,"about_ca_system_score_codex":0.0002473069,"about_ca_system_score_gemma":0.00085209764,"threshold_uncertainty_score":0.0056506395},"labels":[],"label_agreement":null},{"id":"W3046223610","doi":"10.1029/2020jb020103","title":"Well Proximity Governing Stress Drop Variation and Seismic Attenuation Associated With Hydraulic Fracturing Induced Earthquakes","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University; University of Victoria; Geological Survey of Canada","funders":"","keywords":"Hydraulic fracturing; Geology; Attenuation; Drop (telecommunication); Seismology; Geotechnical engineering; Optics","score_opus":0.04560944561614095,"score_gpt":0.28211793520634837,"score_spread":0.23650848959020743,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3046223610","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991304,0.0000133846825,0.00044086616,0.0000051912975,3.390191e-7,0.0000025578754,0.00012682416,0.000013369756,0.0002669813],"genre_scores_gemma":[0.99978226,0.000006135544,0.00008553913,0.0000010422284,2.3197758e-7,8.064439e-7,0.000078401004,0.0000015289451,0.000043962078],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99983466,0.000017062106,0.000009210744,0.000042107025,0.00004948086,0.00004746191],"domain_scores_gemma":[0.9991093,0.00021212368,0.00023577649,0.000054214834,0.0002953909,0.000093088136],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020475274,0.00014562896,0.00022530806,0.0011983801,0.00026974417,0.0005211415,0.00020594102,0.00020075306,0.00091393985],"category_scores_gemma":[0.0016660667,0.00018489947,0.000096035175,0.0012842922,0.0003593531,0.000288277,0.00025603597,0.00015862487,0.00013582339],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007807187,0.000037212685,0.96803546,0.000014420292,0.0000483261,0.00014694958,0.0003025888,0.004689435,0.01951596,0.00008703129,0.00010686905,0.006937651],"study_design_scores_gemma":[8.0561364e-7,0.0000056495355,0.9970932,0.0000010691973,0.0000033598078,0.000013913472,0.000110338144,0.0022753295,0.0004330611,0.000018745992,0.000041543026,0.0000030149367],"about_ca_topic_score_codex":0.17637199,"about_ca_topic_score_gemma":0.2620232,"teacher_disagreement_score":0.17637199,"about_ca_system_score_codex":0.00086933933,"about_ca_system_score_gemma":0.0004551245,"threshold_uncertainty_score":0.35069078},"labels":[],"label_agreement":null},{"id":"W3046336342","doi":"10.1029/2020jb019739","title":"Rise of Great Lakes Surface Water, Sinking of the Upper Midwest of the United States, and Viscous Collapse of the Forebulge of the Former Laurentide Ice Sheet","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"National Aeronautics and Space Administration","keywords":"Geology; Greenland ice sheet; Ice sheet; Hydrology (agriculture); Surface water; Groundwater; Shelf ice; Oceanography; Physical geography; Environmental science; Ice shelf; Sea ice; Geography; Cryosphere","score_opus":0.0372195654071696,"score_gpt":0.27631724052765894,"score_spread":0.23909767512048935,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3046336342","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982874,0.00005256687,0.00002559394,0.0002423106,0.0000022585011,0.000001556167,0.000487122,0.0000060495354,0.00089519174],"genre_scores_gemma":[0.99933463,0.000050930634,0.00004680794,0.000029368304,0.0000033527742,0.0000022188103,0.0003290953,0.000001401745,0.00020228255],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999491,0.000006935489,0.0000037670184,0.000012822557,0.000014193724,0.000013199722],"domain_scores_gemma":[0.9997621,0.000025115645,0.00009436119,0.000009357897,0.000043569195,0.00006545353],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014237156,0.00014544411,0.00008588018,0.00041570136,0.00033559033,0.0005673725,0.00017316957,0.0001611853,0.0011966183],"category_scores_gemma":[0.00047102128,0.00009918678,0.00014218489,0.0005900037,0.00032411216,0.00030992454,0.0005068137,0.00018483214,0.00007962607],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014204411,0.00000637297,0.9958742,0.000007956608,0.000019641926,0.00010400107,0.0002741736,0.0003868319,0.0004319403,0.000113045826,0.0007124301,0.002055316],"study_design_scores_gemma":[9.820562e-7,0.0000034516925,0.99856395,0.000004196399,0.0000045829483,0.000015938454,0.00034159102,0.00060402794,0.00006424956,0.000024095054,0.0003711029,0.0000018134997],"about_ca_topic_score_codex":0.37131378,"about_ca_topic_score_gemma":0.65128213,"teacher_disagreement_score":0.6286862,"about_ca_system_score_codex":0.0012224988,"about_ca_system_score_gemma":0.00076744636,"threshold_uncertainty_score":0.738305},"labels":[],"label_agreement":null},{"id":"W3047310494","doi":"10.1029/2020jb019570","title":"Laramide Orogenesis Driven by Late Cretaceous Weakening of the North American Lithosphere","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"National Science Foundation","keywords":"Geology; Lithosphere; Subduction; Paleontology; Cretaceous; Sedimentary rock; Crust; Thrust fault; North American Plate; Tectonics","score_opus":0.02534534604156916,"score_gpt":0.2651619712229476,"score_spread":0.23981662518137845,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3047310494","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990395,0.000023359993,0.00020265354,0.000015830343,9.709901e-7,0.0000019143147,0.000050388673,0.00001229427,0.0006531624],"genre_scores_gemma":[0.999718,0.000022939364,0.00006454331,0.0000049925475,6.538862e-7,0.0000010186842,0.00004645007,0.0000025962947,0.00013880289],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999572,0.0000042595734,0.0000021046276,0.000013464229,0.0000077543045,0.000015138154],"domain_scores_gemma":[0.99992716,0.000008274642,0.00002416272,0.00000808246,0.000020143703,0.000012169005],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012302061,0.00018082712,0.00013505174,0.00032118076,0.00025435758,0.0003792287,0.00024199646,0.00015934328,0.0013107625],"category_scores_gemma":[0.000240608,0.00015286187,0.00029909462,0.00028254167,0.00030306063,0.00013007919,0.00025915625,0.00014578651,0.000103964005],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029661707,0.0000498661,0.8434579,0.00006196887,0.00017303311,0.00095129467,0.00049022277,0.044074416,0.09631527,0.0011760052,0.00038126833,0.012572051],"study_design_scores_gemma":[0.000010429807,0.000026087664,0.97721946,0.00000679363,0.00003351256,0.00008015092,0.00020943853,0.019194089,0.0024715257,0.0002259962,0.0005148393,0.000007804036],"about_ca_topic_score_codex":0.16913643,"about_ca_topic_score_gemma":0.18207666,"teacher_disagreement_score":0.16913643,"about_ca_system_score_codex":0.0011557896,"about_ca_system_score_gemma":0.00067699805,"threshold_uncertainty_score":0.3363039},"labels":[],"label_agreement":null},{"id":"W3048277231","doi":"10.1029/2019jb018283","title":"Shallow Gas Hydrate Accumulations at a Nigerian Deepwater Pockmark—Quantities and Dynamics","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Methane; Clathrate hydrate; Coring; Pore water pressure; Sediment; Geochemistry; Drilling; Hydrate; Petrology; Geomorphology; Geotechnical engineering","score_opus":0.044785083568540524,"score_gpt":0.31476276050565505,"score_spread":0.2699776769371145,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3048277231","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99937636,0.00003179888,0.000039879487,0.0000069797743,0.000001494954,0.0000024068831,0.00010782814,0.0000038440544,0.00042936296],"genre_scores_gemma":[0.99947625,0.000034981535,0.0001639773,0.0000037163238,0.0000013611435,0.0000033412657,0.00008161649,0.0000010897968,0.00023380895],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995637,0.0000017123939,0.000003872011,0.000013065757,0.000011988966,0.000012963831],"domain_scores_gemma":[0.9999325,0.000006088886,0.000021355612,0.000003025691,0.000018542049,0.000018431067],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000055621218,0.00017221484,0.00017301805,0.0006677372,0.0005108042,0.00041566198,0.0001579097,0.0002544527,0.0005325759],"category_scores_gemma":[0.00009435098,0.00017431148,0.000110836285,0.00044031488,0.00030638004,0.00023579855,0.00046654893,0.00018860583,0.00010662085],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031882085,0.000057051635,0.83469605,0.000112281734,0.00003367135,0.0021214928,0.001079584,0.0011952488,0.14688684,0.00022126744,0.00014359024,0.013134041],"study_design_scores_gemma":[0.0000038926087,0.000047137262,0.9941251,0.000010751283,0.000007637947,0.00014175496,0.0007828285,0.00079508376,0.003565511,0.000031861106,0.00048177727,0.0000065420427],"about_ca_topic_score_codex":0.023270985,"about_ca_topic_score_gemma":0.057952233,"teacher_disagreement_score":0.023270985,"about_ca_system_score_codex":0.0005409427,"about_ca_system_score_gemma":0.00033454958,"threshold_uncertainty_score":0.046271086},"labels":[],"label_agreement":null},{"id":"W3048446177","doi":"10.1029/2020jb020850","title":"Multiple, Coeval Silicic Magma Storage Domains Beneath the Laguna Del Maule Volcanic Field Inferred From Gravity Investigations","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Mira Geoscience (Canada)","funders":"National Science Foundation","keywords":"Geology; Silicic; Rhyolite; Magma; Lava; Volcano; Gravity anomaly; Caldera; Pluton; Magma chamber; Petrology; Geochemistry; Geophysics; Volcanic rock; Seismology; Paleontology","score_opus":0.03869029528822719,"score_gpt":0.29555798952888485,"score_spread":0.25686769424065764,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3048446177","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99922776,0.00006592308,0.00006871357,0.000011619381,5.803876e-7,0.0000022047893,0.00012112975,0.000012515999,0.000489442],"genre_scores_gemma":[0.9997892,0.000015658732,0.000055061257,0.0000013308346,0.0000011411361,7.7134536e-7,0.000080348706,8.2603225e-7,0.00005570467],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996185,0.0000025895015,0.0000025434367,0.000011065436,0.000009536291,0.000012463946],"domain_scores_gemma":[0.99989617,0.000017614975,0.000025651305,0.000007624045,0.000025802537,0.000027158989],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007055283,0.00020424598,0.0000995326,0.0017632432,0.00024873661,0.0005812852,0.00029140033,0.00016068228,0.000891545],"category_scores_gemma":[0.00028135805,0.00010322972,0.00010771205,0.00070148683,0.00032644885,0.0002501343,0.00037163033,0.00008606342,0.000099626224],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000057069654,0.000010186741,0.977732,0.0000203767,0.00002619256,0.00028992174,0.0004050959,0.00074205815,0.013305841,0.00022175883,0.00011240859,0.0070771533],"study_design_scores_gemma":[0.000005323645,0.0000074266536,0.9975247,0.0000039686824,0.0000068900113,0.00007074567,0.00019371441,0.0014625365,0.0004226611,0.000053431737,0.0002455981,0.0000031277802],"about_ca_topic_score_codex":0.038296018,"about_ca_topic_score_gemma":0.051881652,"teacher_disagreement_score":0.038296018,"about_ca_system_score_codex":0.0005727529,"about_ca_system_score_gemma":0.00023426043,"threshold_uncertainty_score":0.076146185},"labels":[],"label_agreement":null},{"id":"W3073392352","doi":"10.1029/2020jb019843","title":"Modeling Geoelectric Fields Induced by Geomagnetic Disturbances in 3D Subsurface Geology, an Example From Southeastern Australia","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Earth's magnetic field; Magnetotellurics; Geology; Geomagnetically induced current; Geophysics; Magnetometer; Magnetic field; Geomagnetic storm; Electrical resistivity and conductivity; Physics","score_opus":0.13869520097215604,"score_gpt":0.3488919017228276,"score_spread":0.21019670075067154,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3073392352","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962943,0.000023670176,0.0021411856,0.000102917744,0.000006705264,0.000013524508,0.00023942765,0.000051387684,0.0011269493],"genre_scores_gemma":[0.9976774,0.00003203881,0.0016654949,0.000014963694,0.0000029258358,0.000009161694,0.00020066524,0.000008003801,0.00038922238],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993217,0.000015808311,0.0000041964663,0.000019646104,0.000011767272,0.000016452375],"domain_scores_gemma":[0.9997987,0.00004809362,0.000031347205,0.00002565722,0.00006037143,0.00003573414],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016091594,0.0004155522,0.0002918911,0.00042575103,0.00034988142,0.00065716024,0.0006190942,0.0007636611,0.00070752564],"category_scores_gemma":[0.0005973485,0.00038172505,0.0006227241,0.0004919537,0.00047346827,0.0003571778,0.000487377,0.00045123431,0.000086797605],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003468263,0.00006299847,0.025966646,0.000010457654,0.00003670756,0.00017080657,0.00005840793,0.9700364,0.0013596587,0.00026412914,0.0001710382,0.0018280214],"study_design_scores_gemma":[0.000013006283,0.000015850963,0.008678776,0.0000023149119,0.000007189803,0.000014344932,0.000040935705,0.99080545,0.00014796655,0.00010795022,0.00016109527,0.0000049748573],"about_ca_topic_score_codex":0.23051503,"about_ca_topic_score_gemma":0.13433447,"teacher_disagreement_score":0.23051503,"about_ca_system_score_codex":0.0011522082,"about_ca_system_score_gemma":0.0010294562,"threshold_uncertainty_score":0.45834655},"labels":[],"label_agreement":null},{"id":"W3080924699","doi":"10.1029/2020jb019383","title":"Diffuse Deformation in the SE Tibetan Plateau: New Insights From Geodetic Observations","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"National Key Research and Development Program of China Stem Cell and Translational Research; National Natural Science Foundation of China","keywords":"Sinistral and dextral; Geology; Seismology; Geodetic datum; Slip (aerodynamics); Crust; Plateau (mathematics); Strike-slip tectonics; Fault (geology); Induced seismicity; Kinematics; Geodesy; Geophysics","score_opus":0.1264117783498151,"score_gpt":0.3189259727181349,"score_spread":0.1925141943683198,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3080924699","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979832,0.00017066387,0.00032825212,0.000028059321,0.0000026649172,0.000004670652,0.00048621275,0.000017742095,0.0009784633],"genre_scores_gemma":[0.9990926,0.000078311445,0.000185833,0.0000073904566,0.000009257324,0.0000028897484,0.0005348256,0.0000030076553,0.00008588142],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992216,0.000009785857,0.000006902159,0.000024052428,0.000022710115,0.00001435524],"domain_scores_gemma":[0.99979585,0.000025406063,0.000058733935,0.000025006288,0.000056946596,0.00003802716],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024955708,0.00027310438,0.00021286582,0.0014822291,0.00025805685,0.00057752314,0.0002695565,0.00033039736,0.0006501647],"category_scores_gemma":[0.00037550283,0.00012507677,0.00019901017,0.0022541187,0.00026679158,0.00029166855,0.00033435063,0.00017242746,0.00013219063],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000065866996,0.00005801931,0.9619102,0.000057669786,0.00006900537,0.0004790895,0.0005576308,0.0036687418,0.014850755,0.00017744514,0.00027944433,0.017826179],"study_design_scores_gemma":[0.0000054044604,0.000016569144,0.9939611,0.0000093460885,0.000009028423,0.000067350964,0.00023465756,0.005105296,0.00013879089,0.00005308931,0.00039512626,0.0000043534533],"about_ca_topic_score_codex":0.017430672,"about_ca_topic_score_gemma":0.035385836,"teacher_disagreement_score":0.017430672,"about_ca_system_score_codex":0.0002748459,"about_ca_system_score_gemma":0.00019880764,"threshold_uncertainty_score":0.034658432},"labels":[],"label_agreement":null},{"id":"W3083022858","doi":"10.1029/2019jb019149","title":"Radon Activity in Volcanic Gases of Mt. Etna by Passive Dosimetry","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Radioactivity and Radon Measurements","field":"Health Professions","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Istituto Nazionale di Geofisica e Vulcanologia; McGill University","keywords":"Radon; Plume; Volcano; Impact crater; Soil gas; Dosimetry; Radionuclide; Environmental science; Atmospheric sciences; Geology; Ground level; Dosimeter; Geochemistry; Nuclear medicine; Meteorology; Astrobiology; Ground floor; Nuclear physics; Geography","score_opus":0.1570452190232572,"score_gpt":0.4744396591685345,"score_spread":0.3173944401452773,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3083022858","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999137,0.00010051223,0.0001717694,0.000003820842,0.0000010954768,0.000004993317,0.00009614058,0.000009188713,0.00047562277],"genre_scores_gemma":[0.99881077,0.000052879142,0.0003950222,0.0000035407836,0.0000036521974,0.000004348697,0.00024479438,0.0000028895174,0.00048201336],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989605,0.00001192082,0.000003810123,0.00003636014,0.000039132407,0.000012803451],"domain_scores_gemma":[0.99992824,0.000012877682,0.000019716883,0.000005319678,0.000025608373,0.000008312141],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012566506,0.00023824736,0.00025439908,0.0007571778,0.00023462523,0.0003231446,0.00028880654,0.0002478673,0.00038433587],"category_scores_gemma":[0.00016036497,0.00012857998,0.00017661357,0.00041227174,0.00017937124,0.00010164931,0.00024456324,0.0001694833,0.00011673419],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004005194,0.0000722282,0.6307468,0.00006972394,0.0000623491,0.00039311516,0.0009476475,0.0010472095,0.34643745,0.00004972923,0.00009659857,0.019676657],"study_design_scores_gemma":[0.0000042051397,0.00014900503,0.98555875,0.000005521814,0.000022181614,0.00011871836,0.0001597035,0.0010684896,0.0121869575,0.000007992351,0.00071421853,0.000004344339],"about_ca_topic_score_codex":0.011841503,"about_ca_topic_score_gemma":0.019755233,"teacher_disagreement_score":0.011841503,"about_ca_system_score_codex":0.00034383291,"about_ca_system_score_gemma":0.00010822321,"threshold_uncertainty_score":0.023545146},"labels":[],"label_agreement":null},{"id":"W3084202746","doi":"10.1029/2020jb019750","title":"A Double Difference Tomography Study of the Washington Forearc: Does Siletzia Control Crustal Seismicity?","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; University of British Columbia","keywords":"Forearc; Geology; Seismology; Induced seismicity; Crust; Seismic tomography; Ridge; Subduction; Tectonics; Geophysics; Paleontology; Mantle (geology)","score_opus":0.04383792682498397,"score_gpt":0.2975117801784116,"score_spread":0.2536738533534276,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3084202746","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983449,0.000038993232,0.0010329257,0.000028800709,9.1062645e-7,0.0000026804291,0.000044616,0.000013497938,0.0004926093],"genre_scores_gemma":[0.9995202,0.000022062664,0.00031357596,0.0000035459518,7.0662156e-7,9.2825206e-7,0.00003410263,0.0000015574203,0.00010325648],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999702,0.000004039502,0.000001345346,0.000010672206,0.0000051903567,0.000008496689],"domain_scores_gemma":[0.9998994,0.000021569467,0.00003493439,0.0000099245335,0.000020811436,0.000013324019],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009228921,0.00016433002,0.000116555115,0.00041849157,0.00014637237,0.00037725148,0.00023655043,0.00020123678,0.0005857937],"category_scores_gemma":[0.0003957249,0.00016000618,0.000098078446,0.0003439811,0.00026101407,0.00028863837,0.00021132105,0.00017553875,0.000062831474],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00059409393,0.00020862614,0.7498197,0.000050742055,0.00014958646,0.0014636515,0.00054173556,0.030434031,0.1730326,0.0020571486,0.00032860617,0.041319504],"study_design_scores_gemma":[0.000020393554,0.00008984031,0.8921772,0.000009696333,0.000040866867,0.00024478417,0.0005405752,0.09718014,0.008534772,0.00050733855,0.0006350005,0.000019350922],"about_ca_topic_score_codex":0.035591938,"about_ca_topic_score_gemma":0.05597429,"teacher_disagreement_score":0.035591938,"about_ca_system_score_codex":0.00038627032,"about_ca_system_score_gemma":0.00034538703,"threshold_uncertainty_score":0.07076955},"labels":[],"label_agreement":null},{"id":"W3086657693","doi":"10.1029/2020jb020918","title":"Crustal Velocity Variations and Constraints on Material Properties in the Charlevoix Seismic Zone, Eastern Canada","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Fonds de recherche du Québec – Nature et technologies","keywords":"Geology; Bouguer anomaly; Seismology; Seismic velocity; Seismic tomography; Impact structure; Tectonics; Gravity anomaly; Fault (geology); Geophysics; Petrology; Mantle (geology); Paleontology; Impact crater","score_opus":0.0445795046145749,"score_gpt":0.27636742034183664,"score_spread":0.23178791572726176,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3086657693","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99786264,0.00009850272,0.00008030018,0.000033746546,9.529882e-7,0.0000050970903,0.0004334938,0.00001261542,0.001472644],"genre_scores_gemma":[0.9991198,0.00005608718,0.00009125301,0.0000059577114,4.6652835e-7,0.0000019442166,0.0002847123,0.0000030459787,0.0004366754],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997489,0.000009657049,0.000008866692,0.00004846323,0.00008737119,0.00009678177],"domain_scores_gemma":[0.99942005,0.000048387727,0.00008638953,0.000019568912,0.0002966995,0.00012892851],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022156253,0.0003409318,0.00025303644,0.0021630216,0.0015599137,0.0014060703,0.0006257697,0.00024735124,0.0014562593],"category_scores_gemma":[0.0007276762,0.0002333509,0.00021680228,0.0022508488,0.00081497454,0.00021773452,0.0007861977,0.0002203438,0.000112208305],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006473538,0.00001964107,0.9848562,0.000020508383,0.000046225658,0.00015046333,0.00061401445,0.002085515,0.003409606,0.00036628256,0.00033345,0.0080333175],"study_design_scores_gemma":[0.0000023797857,0.0000037636821,0.9973214,0.0000069052217,0.0000063150687,0.000015792048,0.0006414153,0.0013928029,0.00017909458,0.000028301445,0.00039620828,0.0000055664796],"about_ca_topic_score_codex":0.9909219,"about_ca_topic_score_gemma":0.9949085,"teacher_disagreement_score":0.015853953,"about_ca_system_score_codex":0.015853953,"about_ca_system_score_gemma":0.010580892,"threshold_uncertainty_score":0.11502904},"labels":[],"label_agreement":null},{"id":"W3087433921","doi":"10.1029/2020jb019396","title":"New Insights Into Crustal and Mantle Flow Beneath the Red River Fault Zone and Adjacent Areas on the Southern Margin of the Tibetan Plateau Revealed by a 3‐D Magnetotelluric Study","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":64,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Fundamental Research Funds for the Central Universities; National Key Research and Development Program of China; National Natural Science Foundation of China","keywords":"Geology; Mantle (geology); Lithosphere; Magnetotellurics; Crust; Transition zone; Petrology; Mantle plume; Upwelling; Hotspot (geology); Geophysics; Geochemistry; Tectonics; Seismology; Electrical resistivity and conductivity","score_opus":0.030014089427154875,"score_gpt":0.276532330162488,"score_spread":0.24651824073533313,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3087433921","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99892575,0.000040264513,0.00048549357,0.000029522073,0.000001063727,0.0000017072276,0.00010709837,0.000022357592,0.00038673898],"genre_scores_gemma":[0.9994505,0.000023236396,0.00030441844,0.000004621358,0.0000025886586,0.0000012240406,0.00011689863,0.000002131455,0.00009438037],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99997616,0.000004947467,0.0000017156938,0.0000064219134,0.0000049989117,0.0000057878556],"domain_scores_gemma":[0.999943,0.000009631156,0.000015316846,0.000006679359,0.000011462625,0.000013931392],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010172728,0.00016720765,0.00015409573,0.0006593566,0.00018920221,0.00046213903,0.00021038859,0.00029684586,0.0007063716],"category_scores_gemma":[0.000163258,0.0001377204,0.00024637635,0.00054008415,0.00021021535,0.00017943914,0.00014986155,0.00015500987,0.00008070216],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026562135,0.00015049483,0.7677259,0.00007712739,0.00018547161,0.0017013949,0.0015041329,0.0527578,0.14945474,0.00093660597,0.00041442623,0.024826383],"study_design_scores_gemma":[0.000018073324,0.000044222572,0.9334907,0.000007300201,0.000023424736,0.00014970006,0.0003667848,0.064116314,0.0010150004,0.00023998666,0.00051198545,0.00001651815],"about_ca_topic_score_codex":0.018889112,"about_ca_topic_score_gemma":0.026048228,"teacher_disagreement_score":0.018889112,"about_ca_system_score_codex":0.000286742,"about_ca_system_score_gemma":0.00016869667,"threshold_uncertainty_score":0.037558317},"labels":[],"label_agreement":null},{"id":"W3088213957","doi":"10.1029/2020jb020949","title":"Reexamining the Potential to Classify Lava Flows From the Fractality of Their Margins","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"National Science Foundation","keywords":"Lava; Geology; Margin (machine learning); Fractal; Flow (mathematics); Scale (ratio); Current meter; Current (fluid); Volcano; Geophysics; Geomorphology; Geometry; Cartography; Mathematics; Seismology; Computer science; Geography; Machine learning; Mathematical analysis","score_opus":0.05713984952833425,"score_gpt":0.32863335567539614,"score_spread":0.2714935061470619,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3088213957","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9864568,0.00015235193,0.010248052,0.00013055358,0.00000651989,0.000021702457,0.0002941504,0.000041766332,0.0026481503],"genre_scores_gemma":[0.9896706,0.00004122791,0.009997375,0.000021602651,0.0000055206488,0.00001274407,0.00014086309,0.000004749534,0.000105384825],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99974364,0.00007715191,0.000016422677,0.000065797976,0.00007060729,0.000026438422],"domain_scores_gemma":[0.9983437,0.0007903285,0.00016073733,0.00018525966,0.0004490325,0.000070853064],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013691338,0.0001792495,0.0002040204,0.0018677954,0.00040905844,0.0012062592,0.0003773928,0.00020802408,0.00045633334],"category_scores_gemma":[0.0029222907,0.000101495505,0.0002009664,0.0006170301,0.00061162905,0.00045079915,0.000632556,0.00026219583,0.000100227306],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020740843,0.000050518865,0.85483164,0.00008139778,0.000056785913,0.00010896351,0.0015197584,0.0052778777,0.027066324,0.0025724235,0.0005277404,0.107699096],"study_design_scores_gemma":[0.000007141902,0.00008345976,0.9350814,0.000056443805,0.00003780387,0.00016587462,0.0016158287,0.05371609,0.0055036684,0.0016040755,0.0021048994,0.000023187278],"about_ca_topic_score_codex":0.015821094,"about_ca_topic_score_gemma":0.023613812,"teacher_disagreement_score":0.015821094,"about_ca_system_score_codex":0.0008093012,"about_ca_system_score_gemma":0.0005059159,"threshold_uncertainty_score":0.03145802},"labels":[],"label_agreement":null},{"id":"W3088302144","doi":"10.1029/2020jb019426","title":"Automatic Detection and Location of Seismic Events From Time‐Delay Projection Mapping and Neural Network Classification","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismology and Earthquake Studies","field":"Computer Science","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"","keywords":"Computer science; Artificial neural network; Data set; Classifier (UML); Data mining; Pattern recognition (psychology); Coherence (philosophical gambling strategy); Artificial intelligence","score_opus":0.05723453526608981,"score_gpt":0.31295595397589954,"score_spread":0.25572141870980974,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3088302144","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6883079,0.00031641932,0.30599394,0.00032751914,0.000068709574,0.00007481364,0.0006580546,0.0017228187,0.0025298148],"genre_scores_gemma":[0.9447243,0.000070348564,0.05377143,0.000020166985,0.000034306966,0.000030778298,0.000500057,0.000025747984,0.0008227498],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997663,0.000051402232,0.000013056474,0.00007186117,0.000058112866,0.00003913714],"domain_scores_gemma":[0.9990915,0.0003912912,0.00018195316,0.00006325345,0.00021376747,0.00005815922],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005415435,0.00059616566,0.000356865,0.0019924329,0.00022714559,0.00058477285,0.00047791583,0.00047543517,0.0012906792],"category_scores_gemma":[0.0020387569,0.00022430535,0.00029132783,0.001176376,0.00024145255,0.0006017585,0.00047942242,0.00051283,0.00035264803],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006127066,0.00041090362,0.11494595,0.00009056283,0.0001651435,0.00029876674,0.00012514427,0.33115038,0.028616576,0.001478868,0.0039305137,0.51817447],"study_design_scores_gemma":[0.000004005374,0.000011025632,0.009673762,0.0000035534722,0.000005555362,0.000013378117,0.0000149806365,0.98790413,0.0018214654,0.00040491254,0.00013849651,0.000004753031],"about_ca_topic_score_codex":0.010219159,"about_ca_topic_score_gemma":0.01279739,"teacher_disagreement_score":0.010219159,"about_ca_system_score_codex":0.000582307,"about_ca_system_score_gemma":0.00049355184,"threshold_uncertainty_score":0.020319343},"labels":[],"label_agreement":null},{"id":"W3088608772","doi":"10.1029/2020jb021040","title":"A Multiscale Numerical Modeling Investigation on the Significance of Flow Partitioning for the Development of Quartz c‐Axis Fabrics","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Composite Material Mechanics","field":"Engineering","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"National Natural Science Foundation of China","keywords":"Microscale chemistry; Vorticity; Quartz; Isotropy; Rheology; Anisotropy; Mechanics; Flow (mathematics); Materials science; Geology; Geometry; Vortex; Physics; Composite material; Optics; Mathematics","score_opus":0.09111291483112745,"score_gpt":0.3182929578218934,"score_spread":0.22718004299076594,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3088608772","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9483527,0.00009087416,0.047640465,0.00020742863,0.00002107871,0.000029623723,0.00013511458,0.00015278967,0.003369951],"genre_scores_gemma":[0.9915422,0.000035060188,0.008167879,0.000011217094,0.0000053776184,0.000017747658,0.000028983291,0.000015952864,0.0001754965],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993813,0.000017139842,0.0000041938383,0.000015763662,0.00001261099,0.000012147873],"domain_scores_gemma":[0.9996697,0.00016269392,0.00006614031,0.00004322606,0.000034787812,0.00002350012],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028942537,0.00022205552,0.00026411115,0.00038119487,0.00028749008,0.00043756378,0.0004581858,0.00044170345,0.0006714842],"category_scores_gemma":[0.0008464048,0.00017646122,0.0004032032,0.00026410283,0.00043799504,0.00039530755,0.00033981376,0.00029063653,0.00005303137],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003140836,0.000063147934,0.0052645826,0.00003144684,0.000021605267,0.00009807921,0.000057239497,0.96628577,0.020563053,0.0050977473,0.000107977205,0.0023778898],"study_design_scores_gemma":[0.0000022607971,0.000005182311,0.0005455073,7.2042263e-7,0.0000013056792,0.0000034398033,0.0000037961775,0.99892396,0.00032304015,0.00015709552,0.000031835305,0.0000017678328],"about_ca_topic_score_codex":0.0061276434,"about_ca_topic_score_gemma":0.0030781825,"teacher_disagreement_score":0.0061276434,"about_ca_system_score_codex":0.00047905173,"about_ca_system_score_gemma":0.0004970981,"threshold_uncertainty_score":0.012183964},"labels":[],"label_agreement":null},{"id":"W3092222650","doi":"10.1029/2020jb020199","title":"Brittle Deformation of Carbonated Peridotite—Insights From Listvenites of the Samail Ophiolite (Oman Drilling Project Hole BT1B)","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Japan Agency for Marine-Earth Science and Technology; National Science Foundation; European Research Council; Alfred P. Sloan Foundation; Deutsche Forschungsgemeinschaft; Japan Society for the Promotion of Science; National Aeronautics and Space Administration","keywords":"Geology; Cataclastic rock; Peridotite; Geochemistry; Ophiolite; Petrology; Metamorphic rock; Shear zone; Mantle (geology); Tectonics; Seismology","score_opus":0.04439866945978643,"score_gpt":0.27653335303610105,"score_spread":0.23213468357631462,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3092222650","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99899656,0.00010430157,0.000066722256,0.000010483273,0.0000012378724,0.000003944537,0.00023789227,0.0000056524987,0.00057326735],"genre_scores_gemma":[0.9993899,0.000055848563,0.00013705603,0.000005551606,0.0000021004967,0.000003261673,0.00016779202,0.0000057689153,0.00023272367],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998932,0.0000065158565,0.000008966022,0.000029222185,0.000034165434,0.000027934522],"domain_scores_gemma":[0.9998851,0.00001257469,0.000040861723,0.000009363673,0.000036584224,0.000015490468],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001494832,0.00024757467,0.00018820773,0.0021899398,0.0006196355,0.0007216185,0.00031315692,0.00037834328,0.0012517209],"category_scores_gemma":[0.00023727643,0.00020250407,0.00015683334,0.0011438864,0.0003706003,0.00033781127,0.0004817372,0.00013376548,0.0001769038],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002319763,0.000043842992,0.7863575,0.00016636329,0.00007598413,0.0010295208,0.0023312212,0.00069123233,0.1913661,0.0001682327,0.00021365462,0.017324323],"study_design_scores_gemma":[0.0000019413112,0.000011719077,0.9976248,0.000005445814,0.000005873047,0.00012242448,0.00028635995,0.00026653198,0.0011792944,0.000013662407,0.00047946643,0.000002408212],"about_ca_topic_score_codex":0.033069078,"about_ca_topic_score_gemma":0.07860585,"teacher_disagreement_score":0.033069078,"about_ca_system_score_codex":0.0006186279,"about_ca_system_score_gemma":0.00024317094,"threshold_uncertainty_score":0.06575316},"labels":[],"label_agreement":null},{"id":"W3093807320","doi":"10.1029/2020jb020059","title":"Earthquake Rupture Through a Step‐Over Fault System: An Exploratory Numerical Study of the Leech River Fault, Southern Vancouver Island","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Seismology; Fault (geology); Offset (computer science); Shear stress; Jump; Slip (aerodynamics); Shear (geology); Engineering; Mechanics; Computer science; Petrology","score_opus":0.04836871349214682,"score_gpt":0.3019546011187073,"score_spread":0.2535858876265605,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3093807320","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99866354,0.000028972794,0.00015599532,0.00005248372,0.0000023484024,0.000008188254,0.000114429415,0.000012037835,0.0009618942],"genre_scores_gemma":[0.99906355,0.00002500604,0.0003343915,0.000014499339,0.0000019234267,0.000007613948,0.00012919497,0.0000045726824,0.00041934446],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998956,0.000019668258,0.0000056943554,0.00002086557,0.00001796578,0.000040129635],"domain_scores_gemma":[0.9994987,0.00021054833,0.00005504778,0.000029053215,0.000074441654,0.00013216551],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019569148,0.00045538013,0.0004969432,0.0005805254,0.0010546036,0.0010126516,0.0011746471,0.0015365346,0.0016979463],"category_scores_gemma":[0.001013263,0.00040221695,0.00050421746,0.0007147272,0.00077957293,0.00035266398,0.00061174715,0.00067968934,0.0001221075],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034069127,0.0005475507,0.10256642,0.00007703115,0.00017433132,0.0015882548,0.00024526907,0.88519716,0.0039427355,0.0010104756,0.00084965175,0.0034604284],"study_design_scores_gemma":[0.00010953091,0.00013563782,0.027422678,0.000013823568,0.00003930948,0.00006787633,0.000551122,0.9707134,0.00043681468,0.00021409882,0.00026985942,0.000025865385],"about_ca_topic_score_codex":0.3133056,"about_ca_topic_score_gemma":0.29515862,"teacher_disagreement_score":0.6866944,"about_ca_system_score_codex":0.0018760016,"about_ca_system_score_gemma":0.0016745795,"threshold_uncertainty_score":0.6229639},"labels":[],"label_agreement":null},{"id":"W3094457323","doi":"10.1029/2020jb020503","title":"Slow Slip and Inter‐transient Locking on the Nicoya Megathrust in the Late and Early Stages of an Earthquake Cycle","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada; Natural Resources Canada","funders":"National Science Foundation","keywords":"Seismology; Slip (aerodynamics); Geology; Subduction; Episodic tremor and slip; Geodesy; Global Positioning System; Slow earthquake; Interplate earthquake; Tectonics; Physics","score_opus":0.05221594364126781,"score_gpt":0.30304174710697895,"score_spread":0.25082580346571115,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3094457323","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993205,0.000073971954,0.00007245188,0.000010939016,0.0000011633327,0.0000025961237,0.00019078283,0.0000035248775,0.00032405998],"genre_scores_gemma":[0.9995277,0.00003199075,0.000042808395,0.0000029042767,0.0000019937781,0.0000031187833,0.00027525582,0.0000010851662,0.00011317319],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998932,0.000021672926,0.000013287835,0.000026334865,0.000020758778,0.000024806317],"domain_scores_gemma":[0.9995018,0.00007120067,0.0002152035,0.000048610324,0.000107559434,0.000055587472],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021560481,0.00016095446,0.00015710187,0.0009965189,0.00018009634,0.00043129156,0.0001746279,0.0001480615,0.00060062396],"category_scores_gemma":[0.0011645989,0.00007621178,0.00013732308,0.0006946017,0.00022352673,0.0001990358,0.00035103076,0.00010234942,0.000096334916],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009109428,0.000017374312,0.9904294,0.000016084172,0.00004381114,0.00011836139,0.00022384191,0.0009163223,0.0024381557,0.00008099366,0.00012095547,0.005503639],"study_design_scores_gemma":[6.822126e-7,0.000007636955,0.99855644,0.0000031497275,0.000005427469,0.000017534743,0.00009686335,0.0010644239,0.000085582105,0.000010763159,0.00014990963,0.0000016443826],"about_ca_topic_score_codex":0.04067013,"about_ca_topic_score_gemma":0.07479924,"teacher_disagreement_score":0.04067013,"about_ca_system_score_codex":0.0004711937,"about_ca_system_score_gemma":0.00020914078,"threshold_uncertainty_score":0.08086681},"labels":[],"label_agreement":null},{"id":"W3096338541","doi":"10.1029/2019jb019065","title":"Localized Afterslip at Geometrical Complexities Revealed by InSAR After the 2016 Central Italy Seismic Sequence","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Institut national des sciences de l'Univers; Agence Nationale de la Recherche; Agence Nationale pour le Développement de la Recherche en Santé; European Space Agency; Université Grenoble Alpes","keywords":"Geology; Seismology; Interferometric synthetic aperture radar; Geodesy; Fault (geology); Sequence (biology); Slip (aerodynamics); Synthetic aperture radar; Remote sensing","score_opus":0.071051130915617,"score_gpt":0.309208079454846,"score_spread":0.23815694853922903,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3096338541","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99314183,0.00016371404,0.00096923485,0.00010028142,0.00003282319,0.000011435215,0.0017705677,0.00011973178,0.003690363],"genre_scores_gemma":[0.9973043,0.000079975696,0.00047942053,0.00001820127,0.00002361087,0.000007249776,0.0016887081,0.000021384987,0.0003770064],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983203,0.000015142553,0.0000080828,0.00004325898,0.000040548082,0.00006092151],"domain_scores_gemma":[0.9996699,0.000035313584,0.00011952049,0.00006402195,0.00007493138,0.000036221936],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020219114,0.00048370907,0.0003270616,0.0013135492,0.0002689799,0.00070599234,0.00027426163,0.00033434457,0.0013223492],"category_scores_gemma":[0.00063419587,0.00019747534,0.00026644714,0.0012740192,0.00036808537,0.0003194024,0.00044363632,0.00027962276,0.0006696484],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007813873,0.00017719208,0.8502736,0.00014682933,0.00020595161,0.0022851715,0.0010027546,0.035700954,0.044557113,0.0009365259,0.009173732,0.05475885],"study_design_scores_gemma":[0.0000070064148,0.000022340979,0.98528117,0.000014250145,0.00002312987,0.000085663945,0.00021793802,0.01160595,0.0007059596,0.00007918058,0.0019426403,0.00001472604],"about_ca_topic_score_codex":0.016749926,"about_ca_topic_score_gemma":0.02419895,"teacher_disagreement_score":0.016749926,"about_ca_system_score_codex":0.00035185297,"about_ca_system_score_gemma":0.0003380648,"threshold_uncertainty_score":0.03330487},"labels":[],"label_agreement":null},{"id":"W3097748295","doi":"10.1029/2020jb020459","title":"Integrating Magnetotelluric and Seismic Images of Silicic Magma Systems: A Case Study From the Laguna del Maule Volcanic Field, Central Chile","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"National Science Foundation","keywords":"Magnetotellurics; Geology; Silicic; Volcano; Magma; Geophysics; Magma chamber; Seismology; Volcanism; Petrology; Mineralogy; Electrical resistivity and conductivity; Tectonics","score_opus":0.0392684613396044,"score_gpt":0.31594458088732313,"score_spread":0.27667611954771876,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3097748295","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984712,0.000086862245,0.00022426617,0.00005459718,0.0000014656025,0.000018104569,0.00031139603,0.000016391561,0.0008158069],"genre_scores_gemma":[0.9984993,0.00008531733,0.0007869848,0.000009045717,0.0000038778126,0.000009966281,0.00029301122,0.0000071786767,0.0003053493],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998522,0.00003354861,0.000012927027,0.000031795465,0.00003442102,0.000035080637],"domain_scores_gemma":[0.9994856,0.00020854738,0.00007907304,0.000052668223,0.00011818693,0.00005586217],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038190177,0.00036576745,0.00021184335,0.0018315973,0.00042054476,0.00091973547,0.0007703937,0.00047403682,0.0007100858],"category_scores_gemma":[0.0012038528,0.00025169598,0.0002939695,0.0024278564,0.0005767659,0.00045011262,0.0006182789,0.0002116701,0.00011090986],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00051353895,0.00050745637,0.8429537,0.000449417,0.00030750324,0.025255721,0.006461636,0.036366034,0.026866306,0.0009789522,0.001660577,0.057679135],"study_design_scores_gemma":[0.00007821372,0.00010588615,0.9461336,0.00008832661,0.00009732927,0.0013863647,0.009204283,0.03610651,0.0034542605,0.00035497893,0.0029385036,0.000051680487],"about_ca_topic_score_codex":0.13801001,"about_ca_topic_score_gemma":0.22062567,"teacher_disagreement_score":0.13801001,"about_ca_system_score_codex":0.0018175461,"about_ca_system_score_gemma":0.00089125667,"threshold_uncertainty_score":0.2744134},"labels":[],"label_agreement":null},{"id":"W3104635880","doi":"10.1029/2020jb021290","title":"Geochemical and C‐O Isotopic Study of Ophiolite‐Derived Carbonates of the Barzaman Formation, Oman: Evidence of Natural CO<sub>2</sub> Sequestration Via Carbonation of Ultramafic Clasts","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Regina","funders":"Universidade Federal de Ouro Preto","keywords":"Calcite; Ophiolite; Carbonate; Geology; Dolomite; Geochemistry; Isotopic signature; Alkalinity; Ultramafic rock; Diagenesis; Mineralogy; Environmental chemistry; Stable isotope ratio; Chemistry","score_opus":0.03035038890933772,"score_gpt":0.2930673764287016,"score_spread":0.2627169875193639,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3104635880","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999673,0.000025278145,0.000018872335,0.0000039638517,5.8189016e-7,0.000001827554,0.00006324924,0.0000010685505,0.00021214197],"genre_scores_gemma":[0.9994796,0.00003786349,0.00011056014,0.000007689523,0.0000021981994,0.0000032220787,0.00015400269,0.0000018945218,0.00020312949],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991584,0.0000052387027,0.000006425214,0.000021345259,0.000028202463,0.00002290383],"domain_scores_gemma":[0.99991953,0.0000060644556,0.000022343753,0.000003637277,0.00003220352,0.000016316915],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009980376,0.00026292627,0.00018466392,0.0012706551,0.00067891314,0.00041620753,0.00021246455,0.0002255492,0.00045602326],"category_scores_gemma":[0.00017346557,0.00017789078,0.00012657931,0.00069885585,0.0003189505,0.00015829172,0.00029861595,0.00015769107,0.00010350847],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025037222,0.000076246135,0.618008,0.00008132405,0.00008216042,0.0005520445,0.0008843694,0.00031208276,0.37229332,0.00011721936,0.00008237916,0.0072605065],"study_design_scores_gemma":[0.0000035243713,0.000027397136,0.99579996,0.000002765121,0.000008210053,0.00008836392,0.00022143852,0.000286274,0.0032184934,0.000007048114,0.00033407324,0.0000025806378],"about_ca_topic_score_codex":0.04384408,"about_ca_topic_score_gemma":0.0727757,"teacher_disagreement_score":0.04384408,"about_ca_system_score_codex":0.0006261667,"about_ca_system_score_gemma":0.00043364184,"threshold_uncertainty_score":0.08717775},"labels":[],"label_agreement":null},{"id":"W3106468226","doi":"10.1029/2020jb020529","title":"Strain Accumulation and Release Rate in Canada: Implications for Long‐Term Crustal Deformation and Earthquake Hazards","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada; Natural Resources Canada","funders":"Natural Resources Canada","keywords":"Geology; Post-glacial rebound; Geodetic datum; Seismology; Seismic hazard; Crust; Deformation (meteorology); Strain rate; Continental crust; Seismic moment; Geodesy; Glacial period; Geophysics; Tectonics; Geomorphology; Fault (geology); Oceanography","score_opus":0.06541004199429959,"score_gpt":0.34333209228399403,"score_spread":0.2779220502896944,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3106468226","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9916814,0.00041693522,0.00036008828,0.00060857984,0.0000052299083,0.0000138211535,0.0039022292,0.000027243133,0.0029845566],"genre_scores_gemma":[0.9980185,0.0001835929,0.00020697512,0.00004099923,0.0000015910368,0.0000032091345,0.00089510425,0.000005478155,0.0006445934],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996712,0.000018977216,0.000023110088,0.00005155621,0.00012374617,0.00011149786],"domain_scores_gemma":[0.9980696,0.0001985803,0.00037599166,0.00006819119,0.0009773542,0.00031044247],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005613222,0.00026236888,0.00028048203,0.0014661736,0.0011263518,0.0014711749,0.0009661885,0.00028971166,0.0018508919],"category_scores_gemma":[0.0023147715,0.00017490837,0.00039297648,0.0036038358,0.00070121145,0.00046063666,0.0006506584,0.0004376768,0.000114167015],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009897487,0.000026449829,0.9828318,0.00003135153,0.00008878288,0.00014110914,0.00036251303,0.004027863,0.0009809963,0.0007444106,0.0007152516,0.009950534],"study_design_scores_gemma":[0.0000025853685,0.000005931415,0.9948009,0.000013530934,0.000015985463,0.000027208169,0.0006245647,0.003644555,0.00018443612,0.00011881704,0.00055158633,0.000009803977],"about_ca_topic_score_codex":0.9950964,"about_ca_topic_score_gemma":0.99537045,"teacher_disagreement_score":0.02379708,"about_ca_system_score_codex":0.02379708,"about_ca_system_score_gemma":0.018270543,"threshold_uncertainty_score":0.17266071},"labels":[],"label_agreement":null},{"id":"W3106545159","doi":"10.1029/2020jb020574","title":"Variations in Seismic Wave Speed and <i>V</i><sub><i>P</i></sub>/<i>V</i><sub><i>S</i></sub> Ratio in the North American Lithosphere","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Lithosphere; Geology; Rayleigh wave; P wave; Mantle (geology); Seismology; Tectonics; Mineralogy; Geometry; Geophysics; Wave propagation; Physics; Optics; Mathematics","score_opus":0.028966227016934368,"score_gpt":0.2674094895166785,"score_spread":0.23844326249974412,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3106545159","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994281,0.000008097747,0.00021530957,0.00001496233,4.7720545e-7,9.990828e-7,0.00007419988,0.000011739556,0.00024610097],"genre_scores_gemma":[0.99969196,0.000010389694,0.00011582789,0.0000019876675,7.177548e-7,0.0000011862477,0.00010825236,0.0000028029294,0.00006694321],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994755,0.00000961733,0.0000028811928,0.00001922242,0.000008705669,0.00001204358],"domain_scores_gemma":[0.99987423,0.000044849872,0.000028711118,0.000013719094,0.000022475968,0.000015926362],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016870421,0.00022751883,0.000096353746,0.0004485347,0.00020505127,0.0004337607,0.00025251682,0.00023551927,0.00070146646],"category_scores_gemma":[0.00048365933,0.00027826114,0.0002513248,0.00031857,0.00030188265,0.00020706907,0.00013473132,0.00019833392,0.000100152494],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015550954,0.00009228093,0.7493563,0.00002212154,0.00014924872,0.00015815184,0.00018463269,0.20976593,0.02566217,0.0008648919,0.00070333196,0.01288546],"study_design_scores_gemma":[0.000011937808,0.000027834061,0.72300255,0.0000043653254,0.00002845353,0.00005204771,0.00015494405,0.27453175,0.001650539,0.00031922304,0.00019922359,0.000017152648],"about_ca_topic_score_codex":0.06660458,"about_ca_topic_score_gemma":0.06802922,"teacher_disagreement_score":0.06660458,"about_ca_system_score_codex":0.0006759968,"about_ca_system_score_gemma":0.00034341178,"threshold_uncertainty_score":0.13243383},"labels":[],"label_agreement":null},{"id":"W3106682895","doi":"10.1029/2020jb020887","title":"Statistics and Forecasting of Aftershocks During the 2019 Ridgecrest, California, Earthquake Sequence","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Aftershock; Foreshock; Sequence (biology); Seismology; Geology; Extreme value theory; Induced seismicity; Statistics; Mathematics","score_opus":0.058773026645371755,"score_gpt":0.31158267569495046,"score_spread":0.2528096490495787,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3106682895","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9950813,0.000052540454,0.003771415,0.000053553482,0.0000052222567,0.0000113417655,0.0005867835,0.000043572898,0.00039435306],"genre_scores_gemma":[0.99796474,0.00003607807,0.0008726968,0.0000028864863,0.000005511533,0.000004517108,0.00094226096,0.0000025295608,0.00016884563],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997713,0.000052644657,0.000018572982,0.000060708793,0.00006971118,0.000027097389],"domain_scores_gemma":[0.9958658,0.0023300925,0.0008145913,0.00016329493,0.00064280105,0.00018337186],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013391785,0.00026329406,0.0002748912,0.0013118951,0.00018207419,0.0004502184,0.00031310858,0.00031524632,0.0004890272],"category_scores_gemma":[0.0047951215,0.00013926163,0.0002074206,0.00082511955,0.00027732068,0.0003175227,0.00022368728,0.00029204867,0.00010296094],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028851366,0.00008472358,0.4883736,0.000044271717,0.000078418096,0.0002411813,0.00008032751,0.48637727,0.0017619566,0.0015625128,0.0012216961,0.019885404],"study_design_scores_gemma":[0.000010779674,0.00010738883,0.29565606,0.0000106521875,0.000024923675,0.000034732202,0.000121954705,0.70250505,0.00071825105,0.0005183069,0.00027473585,0.000017127977],"about_ca_topic_score_codex":0.033293556,"about_ca_topic_score_gemma":0.030318342,"teacher_disagreement_score":0.033293556,"about_ca_system_score_codex":0.0005314228,"about_ca_system_score_gemma":0.0006895081,"threshold_uncertainty_score":0.06619948},"labels":[],"label_agreement":null},{"id":"W3107910832","doi":"10.1029/2020jb020988","title":"Multiple Episodes of Fluid Infiltration Along a Single Metasomatic Channel in Metacarbonates (Mogok Metamorphic Belt, Myanmar) and Implications for CO<sub>2</sub> Release in Orogenic Belts","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Metasomatism; Geology; Geochemistry; Baddeleyite; Metamorphic rock; Calcite; Infiltration (HVAC); Dolomite; Dissolution; Zircon; Mineralogy; Mantle (geology); Chemistry; Materials science","score_opus":0.05676603048280317,"score_gpt":0.2901672017927506,"score_spread":0.23340117130994742,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3107910832","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997608,0.00003148978,0.000036835478,0.0000074640866,5.12748e-7,0.0000019641323,0.00002954103,0.0000034690445,0.00012798785],"genre_scores_gemma":[0.9998381,0.000014871982,0.000047637386,0.0000023131574,0.0000010384925,0.000001535693,0.00003075384,0.0000014416186,0.00006227174],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998969,0.000006704041,0.000008395626,0.00004461293,0.000011366856,0.000032157157],"domain_scores_gemma":[0.9998822,0.000008723117,0.00006993728,0.000007922865,0.000014593213,0.000016622893],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012074586,0.00016667614,0.00021020613,0.0007770983,0.00044107484,0.00049536803,0.00025286208,0.00031802926,0.0009614327],"category_scores_gemma":[0.00023773476,0.00021754981,0.0001626759,0.0004497838,0.00060223043,0.00036476547,0.0005079207,0.00014734647,0.00010100099],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021223318,0.000028160108,0.8940351,0.000051590912,0.00004573383,0.0008917073,0.0012870653,0.0006187548,0.09726172,0.00020672489,0.00006408113,0.0052972143],"study_design_scores_gemma":[0.000003418243,0.000025051164,0.99768436,0.0000025929412,0.000008181496,0.0001376569,0.00032135317,0.00046985186,0.0011197886,0.000022565031,0.00020247247,0.000002677665],"about_ca_topic_score_codex":0.009177137,"about_ca_topic_score_gemma":0.013216658,"teacher_disagreement_score":0.009177137,"about_ca_system_score_codex":0.0004893202,"about_ca_system_score_gemma":0.00020225997,"threshold_uncertainty_score":0.018247485},"labels":[],"label_agreement":null},{"id":"W3113053351","doi":"10.1029/2020jb020107","title":"Laboratory Experiments Contrasting Growth of Uniformly and Nonuniformly Spaced Hydraulic Fractures","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Hydraulic Fracturing and Reservoir Analysis","field":"Engineering","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"National Science Foundation","keywords":"Fracture (geology); Geology; Mechanics; Hydraulic fracturing; Planar; Wellbore; Geotechnical engineering; Materials science; Petroleum engineering; Physics; Computer science","score_opus":0.02236969039829987,"score_gpt":0.30482958027870016,"score_spread":0.28245988988040027,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3113053351","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99707437,0.000032242122,0.0023236491,0.0000146094235,0.00000938882,0.000017519425,0.00008905095,0.00005056898,0.00038859277],"genre_scores_gemma":[0.9969766,0.00004925559,0.0025223575,0.000009238793,0.0000025437012,0.00003180013,0.00006339766,0.0000076149818,0.00033712725],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99981076,0.00001857382,0.000014750187,0.000052302934,0.000054527707,0.000049198297],"domain_scores_gemma":[0.9993399,0.0002604673,0.00017413325,0.00007386441,0.00008263433,0.00006891404],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022571142,0.00034910627,0.00018688018,0.00017017768,0.00020829878,0.00023414585,0.00050803565,0.0003944908,0.0009650191],"category_scores_gemma":[0.0005273364,0.00017506153,0.00019636493,0.0001163255,0.0003771578,0.0002383228,0.0003719869,0.0004647122,0.00010665777],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002370686,0.00057382014,0.0029721386,0.00006145993,0.000010135672,0.00014633342,0.00008625138,0.019305395,0.97248995,0.0002593944,0.00012380806,0.0037343109],"study_design_scores_gemma":[0.000055292963,0.00385398,0.005254109,0.000010572651,0.000020213072,0.000087023975,0.00013867918,0.05601307,0.93375134,0.00017992106,0.0006102518,0.000025537393],"about_ca_topic_score_codex":0.0011311527,"about_ca_topic_score_gemma":0.0018122921,"teacher_disagreement_score":0.0011311527,"about_ca_system_score_codex":0.00028899687,"about_ca_system_score_gemma":0.00026263867,"threshold_uncertainty_score":0.0032283664},"labels":[],"label_agreement":null},{"id":"W3121785412","doi":"10.1029/2021jb021702","title":"Structural and Thermal Evolution of an Infant Subduction Shear Zone: Insights From Sub‐Ophiolite Metamorphic Rocks Recovered From Oman Drilling Project Site BT‐1B","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Geology; Subduction; Ophiolite; Geochemistry; Metamorphic facies; Greenschist; Metamorphic rock; Shear zone; Amphibole; Blueschist; Petrology; Seismology; Geomorphology; Paleontology; Facies; Tectonics; Eclogite; Quartz","score_opus":0.027474629990329603,"score_gpt":0.26884935646752744,"score_spread":0.24137472647719785,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3121785412","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998679,0.00010538799,0.00007044981,0.000010801088,0.0000013649017,0.0000043888094,0.000543811,0.0000058589067,0.0005789978],"genre_scores_gemma":[0.9984717,0.00009573367,0.00024544421,0.000013075243,0.0000043218806,0.0000086807995,0.0007144967,0.000009247142,0.0004372895],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984527,0.0000094125135,0.000012468235,0.000047467303,0.000043637447,0.000041749125],"domain_scores_gemma":[0.99982685,0.00001110892,0.000060369097,0.000013221691,0.000066668144,0.000021766664],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022285704,0.00036459824,0.00025548314,0.0022725372,0.00084113976,0.00066702865,0.00032758244,0.00042704586,0.0011336014],"category_scores_gemma":[0.0002523503,0.0002503371,0.00017404559,0.001777257,0.00038531885,0.00032832558,0.00059209083,0.00018496384,0.00039533334],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015514946,0.00004909213,0.8971899,0.0000882689,0.00007023872,0.00044380515,0.0019218936,0.00045038154,0.08537183,0.00010533197,0.00032088842,0.01383326],"study_design_scores_gemma":[0.0000016662262,0.000011064019,0.99803704,0.000006983368,0.00000821299,0.000076522934,0.00034675497,0.00022458914,0.0007501227,0.0000072407115,0.00052782276,0.0000019908712],"about_ca_topic_score_codex":0.04532275,"about_ca_topic_score_gemma":0.10974019,"teacher_disagreement_score":0.04532275,"about_ca_system_score_codex":0.0007260342,"about_ca_system_score_gemma":0.00032796085,"threshold_uncertainty_score":0.09011787},"labels":[],"label_agreement":null},{"id":"W3124276329","doi":"10.1029/2020jb020311","title":"Large‐Scale Fracture Systems Are Permeable Pathways for Fault Activation During Hydraulic Fracturing","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":78,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Natural Environment Research Council; Sight Research UK","keywords":"Hydraulic fracturing; Induced seismicity; Geology; Seismology; Microseism; Fracture (geology); Fault (geology); Pore water pressure; Seismometer; Petrology; Geotechnical engineering","score_opus":0.04106879206607408,"score_gpt":0.3010435762335246,"score_spread":0.25997478416745057,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3124276329","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990326,0.000021625856,0.0005779208,0.000008343634,3.9321174e-7,0.0000028506204,0.000047228725,0.000010322517,0.0002988602],"genre_scores_gemma":[0.99978095,0.000006521049,0.00015489191,7.537081e-7,2.7085275e-7,0.000001003044,0.000018419521,4.3046398e-7,0.000036803423],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994195,0.000005322223,0.00000302458,0.000014342141,0.000014130752,0.000021261116],"domain_scores_gemma":[0.9996753,0.00007945,0.00013286123,0.000021402428,0.000047282545,0.00004364359],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008420223,0.000091580674,0.000094343064,0.00048767927,0.00023017246,0.0003754225,0.00020583953,0.00018451009,0.0008010917],"category_scores_gemma":[0.000459117,0.00012024535,0.000080788865,0.0003867143,0.0005065768,0.00021068005,0.00029102774,0.000121063604,0.000052026488],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032666733,0.00008828244,0.79962796,0.000075827615,0.000063747444,0.000972186,0.00088937144,0.014587708,0.1609474,0.001864959,0.00022861104,0.020327302],"study_design_scores_gemma":[0.000005231538,0.00003657677,0.9865807,0.0000057055327,0.000010827859,0.00016421141,0.00046460162,0.008789607,0.0032455665,0.0004526712,0.00023629286,0.0000079288375],"about_ca_topic_score_codex":0.017501798,"about_ca_topic_score_gemma":0.04028007,"teacher_disagreement_score":0.017501798,"about_ca_system_score_codex":0.0005141167,"about_ca_system_score_gemma":0.00035893693,"threshold_uncertainty_score":0.034799874},"labels":[],"label_agreement":null},{"id":"W3127243155","doi":"10.1029/2020jb021037","title":"One and a Half Million Yearlong Aridity During the Middle Eocene in North‐West China Linked to a Global Cooling Episode","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Aridification; Geology; Global cooling; Plateau (mathematics); Paleoclimatology; Paleontology; Arid; Sedimentary rock; Magnetostratigraphy; Climatology; Climate change; Oceanography; Structural basin","score_opus":0.05101169092289276,"score_gpt":0.30743379472955973,"score_spread":0.25642210380666697,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3127243155","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996736,0.000044114408,0.000040833605,0.000010584358,8.9452095e-7,5.865337e-7,0.000068636924,0.0000034769355,0.00015713785],"genre_scores_gemma":[0.99980074,0.000020824371,0.000023084995,0.0000030669319,0.0000012098013,7.2694036e-7,0.00009198954,5.371083e-7,0.000057767964],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995446,0.000006603217,0.0000034612162,0.00001651731,0.000006491712,0.000012575394],"domain_scores_gemma":[0.9998907,0.000010342867,0.000041115094,0.000012012991,0.000019177089,0.000026662285],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019919263,0.00013975623,0.00010252896,0.0005747111,0.00033175462,0.000259519,0.00016121988,0.00014012572,0.00074625725],"category_scores_gemma":[0.00024527474,0.000085922205,0.00012035697,0.00049194315,0.00029197516,0.00016552315,0.00028127225,0.00011057174,0.00007142739],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006972068,0.000010783693,0.98215,0.00002165974,0.000045295437,0.00017033424,0.0009655219,0.0007512991,0.00684528,0.00018189798,0.00016137291,0.00862684],"study_design_scores_gemma":[0.0000013864164,0.000009235696,0.99885476,0.0000026507666,0.0000069260686,0.000026923703,0.00010905847,0.00058410544,0.00013072147,0.00003114204,0.00024142022,0.0000015832708],"about_ca_topic_score_codex":0.030796258,"about_ca_topic_score_gemma":0.04716522,"teacher_disagreement_score":0.030796258,"about_ca_system_score_codex":0.00048681817,"about_ca_system_score_gemma":0.00029174474,"threshold_uncertainty_score":0.061233997},"labels":[],"label_agreement":null},{"id":"W3128179381","doi":"10.1029/2020jb020384","title":"Fluid‐Earthquake and Earthquake‐Earthquake Interactions in Southern Kansas, USA","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Induced seismicity; Geology; Seismology; Pore water pressure; Intraplate earthquake; Fault (geology); Poromechanics; Tectonics; Geotechnical engineering; Porosity","score_opus":0.05371020253437864,"score_gpt":0.3304158486741582,"score_spread":0.27670564613977955,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3128179381","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987431,0.000039311246,0.00006512563,0.000032220494,0.0000013251384,0.000003314861,0.0007980782,0.000010927515,0.00030673016],"genre_scores_gemma":[0.99897456,0.000025599618,0.000059206464,0.0000061617225,0.0000012536913,0.000002851733,0.00062421255,0.0000014587523,0.0003046733],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999356,0.0000073519514,0.0000046411974,0.000018006675,0.000013545385,0.000020820806],"domain_scores_gemma":[0.9994229,0.00005661486,0.00026699097,0.000016598246,0.00015484987,0.000082002916],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009250763,0.00013841936,0.000117666474,0.0010649876,0.00038820156,0.00045857838,0.00024530655,0.0002380364,0.0015176494],"category_scores_gemma":[0.0004694287,0.00012768866,0.00011308212,0.0016914498,0.00024345604,0.00024627557,0.00043990734,0.00019056391,0.00021832739],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000040084888,0.000031683638,0.9948185,0.000022589355,0.000030788568,0.000118201824,0.00048394856,0.00063901226,0.0008783407,0.000041550004,0.00044315524,0.0024520678],"study_design_scores_gemma":[0.0000015400738,0.000009158307,0.9984049,0.0000041559233,0.000005566647,0.000015916356,0.000485311,0.000718764,0.00004845239,0.00000963754,0.00029415157,0.000002469869],"about_ca_topic_score_codex":0.2816116,"about_ca_topic_score_gemma":0.5007689,"teacher_disagreement_score":0.2816116,"about_ca_system_score_codex":0.00096926145,"about_ca_system_score_gemma":0.0007131575,"threshold_uncertainty_score":0.55994487},"labels":[],"label_agreement":null},{"id":"W3128214727","doi":"10.1029/2020jb021074","title":"What Controls Effective Elastic Thickness of the Lithosphere in the Pacific Ocean?","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Geology; Lithosphere; Seamount; Subduction; Bathymetry; Seismology; Seafloor spreading; Oceanic crust; Mantle (geology); Pacific Plate; Ridge push; Mid-ocean ridge; Geophysics; Tectonics; Oceanography","score_opus":0.024284041419390816,"score_gpt":0.30271724833223573,"score_spread":0.2784332069128449,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3128214727","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982973,0.0001357939,0.0006087451,0.0000422958,0.0000028605002,0.0000019198155,0.00014204095,0.000015419833,0.000753671],"genre_scores_gemma":[0.9996774,0.000057579015,0.00009562294,0.0000060393613,0.000002136123,0.0000011103843,0.0000638637,0.0000053346907,0.00009091243],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992096,0.000013575836,0.000006779563,0.000023824767,0.000012493532,0.000022307631],"domain_scores_gemma":[0.9995921,0.00011148553,0.00013918796,0.00003296587,0.000057570975,0.000066708955],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022025286,0.00019323823,0.0001350757,0.0005728391,0.00018604686,0.0007479827,0.00023292235,0.00024558292,0.0013619304],"category_scores_gemma":[0.0012936963,0.00023102202,0.00014009565,0.00042295843,0.0004375936,0.00050550065,0.00035054135,0.00016086102,0.00016105027],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018476216,0.000030976338,0.8679631,0.00012132644,0.00019648821,0.0004088142,0.00033520843,0.01175879,0.102927364,0.00093194743,0.00027788297,0.014863369],"study_design_scores_gemma":[0.0000032082946,0.000013913382,0.9886115,0.000013007008,0.000022067863,0.000072611845,0.000282876,0.0074691297,0.0027804708,0.00048273813,0.00023678264,0.0000117575455],"about_ca_topic_score_codex":0.005573716,"about_ca_topic_score_gemma":0.004254326,"teacher_disagreement_score":0.005573716,"about_ca_system_score_codex":0.00021293058,"about_ca_system_score_gemma":0.0002183607,"threshold_uncertainty_score":0.01108253},"labels":[],"label_agreement":null},{"id":"W3129103754","doi":"10.1029/2020jb020678","title":"Balanced Cross‐Sections and Numerical Modeling of the Lithospheric‐Scale Evolution of the Hindu Kush and Pamir","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Magmatism; Subduction; Lithosphere; Crust; Terrane; Mantle (geology); Seismology; Metamorphism; Continental crust; Delamination (geology); Geochemistry; Tectonics","score_opus":0.021993263609231303,"score_gpt":0.29388181751759584,"score_spread":0.2718885539083645,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3129103754","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99030465,0.00006970526,0.0043289284,0.00014370187,0.00001943946,0.000018120916,0.00042508767,0.00014695807,0.004543454],"genre_scores_gemma":[0.99768114,0.000030096442,0.0013317182,0.000020203886,0.000005149758,0.000016105716,0.00017437123,0.000018740291,0.000722472],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999242,0.000019677938,0.000004281147,0.000019300627,0.000010595739,0.00002192107],"domain_scores_gemma":[0.999678,0.0001209706,0.00006003615,0.000031086223,0.000046550736,0.00006322821],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025795057,0.00053981086,0.0003407893,0.0005795822,0.0006124878,0.0010700083,0.0009550646,0.001240422,0.0028174813],"category_scores_gemma":[0.00091718324,0.0005572973,0.00069039775,0.00055404933,0.0007690903,0.00036592668,0.00073490513,0.00050680037,0.00025313802],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000033624823,0.00002320176,0.0044026393,0.000006364415,0.000018176705,0.00004786796,0.000018812001,0.9935354,0.0007337679,0.0005313859,0.00006953942,0.000579182],"study_design_scores_gemma":[0.000013108099,0.0000101674,0.001732167,0.0000016003341,0.0000051538213,0.0000053262474,0.000013254242,0.9979296,0.00011591616,0.00010751485,0.000062177365,0.000004000551],"about_ca_topic_score_codex":0.062457852,"about_ca_topic_score_gemma":0.023998456,"teacher_disagreement_score":0.062457852,"about_ca_system_score_codex":0.0013332538,"about_ca_system_score_gemma":0.0008062,"threshold_uncertainty_score":0.1241886},"labels":[],"label_agreement":null},{"id":"W3131278847","doi":"10.1029/2020jb020823","title":"Linking the Siberian Flood Basalts and Giant Ni‐Cu‐PGE Sulfide Deposits at Norilsk","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"National Natural Science Foundation of China","keywords":"Flood basalt; Geology; Geochemistry; Basalt; Sill; Sulfide; Crust; Large igneous province; Igneous rock; Magma chamber; Volcano; Mantle (geology); Mafic; Magma; Volcanism; Magmatism; Tectonics; Paleontology","score_opus":0.028529486459544565,"score_gpt":0.27562015980843746,"score_spread":0.2470906733488929,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3131278847","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985252,0.000069778915,0.0000874713,0.000024200399,0.000003241932,0.0000030683752,0.00022021595,0.0000208243,0.0010460177],"genre_scores_gemma":[0.9994772,0.000028427314,0.00006650819,0.000003132958,8.5450665e-7,0.0000013313562,0.0002266396,0.000004024663,0.00019198935],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990046,0.000010610453,0.0000098998435,0.000036852394,0.000016330365,0.000025810696],"domain_scores_gemma":[0.99988353,0.00001205637,0.000027573758,0.000019402043,0.000029958677,0.000027541826],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022444825,0.00033432353,0.00033442967,0.0008168673,0.0005807381,0.0009029094,0.0003749418,0.0003267484,0.0022964976],"category_scores_gemma":[0.00028696514,0.00023409832,0.0003214347,0.00059956615,0.00034910245,0.00043436568,0.00096690987,0.00022554169,0.00030364515],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022656114,0.000052401036,0.9573819,0.000106161555,0.00019546573,0.0011531011,0.0006523825,0.010654912,0.016041959,0.00036156457,0.0002491823,0.012924413],"study_design_scores_gemma":[0.000012104943,0.00002666657,0.97879237,0.000018225805,0.00004679089,0.00012522584,0.00060716626,0.01711951,0.0022435877,0.0001372754,0.00086011284,0.000010942927],"about_ca_topic_score_codex":0.06679239,"about_ca_topic_score_gemma":0.058372427,"teacher_disagreement_score":0.06679239,"about_ca_system_score_codex":0.0013323721,"about_ca_system_score_gemma":0.000938297,"threshold_uncertainty_score":0.13280725},"labels":[],"label_agreement":null},{"id":"W3134518932","doi":"10.1029/2020jb020924","title":"Lithospheric Structure and Flat‐Slab Subduction in the Northern Appalachians: Evidence From Rayleigh Wave Tomography","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Natural Environment Research Council; Sight Research UK","keywords":"Geology; Lithosphere; Subduction; Seismology; Terrane; Tectonics; Seismic tomography; Proterozoic; Geophysics; Paleontology; Mantle (geology)","score_opus":0.03367875215959434,"score_gpt":0.2860005344117303,"score_spread":0.252321782252136,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3134518932","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994609,0.00006152545,0.000057872265,0.000016265225,5.715206e-7,0.0000013982475,0.000060665578,0.0000030070714,0.0003377516],"genre_scores_gemma":[0.9997435,0.000063150146,0.000062607585,0.0000032144756,0.0000011107924,0.0000012268575,0.00007406569,9.71769e-7,0.000050223767],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999201,0.000013725966,0.000008932977,0.000016214977,0.000020316698,0.000020699497],"domain_scores_gemma":[0.99959403,0.00008607477,0.00014240571,0.000031996686,0.00011179876,0.000033762317],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019967924,0.00020038876,0.00013546497,0.0011057936,0.00039369956,0.00072161364,0.0002817817,0.00019540192,0.00063330104],"category_scores_gemma":[0.0008540566,0.00017570102,0.00011435485,0.0014189078,0.000608643,0.00029798032,0.00044918995,0.00015576833,0.00012224684],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000062339095,0.000014827972,0.98449796,0.00001622753,0.000037519152,0.000512684,0.0009442111,0.0007377722,0.006370645,0.00008824913,0.00005400012,0.0066636563],"study_design_scores_gemma":[0.0000016944887,0.0000062563577,0.99835473,0.0000045091615,0.000008328175,0.000093413866,0.0005680229,0.0006435226,0.0001958092,0.000027083004,0.000093843715,0.0000027874455],"about_ca_topic_score_codex":0.11891607,"about_ca_topic_score_gemma":0.15230477,"teacher_disagreement_score":0.11891607,"about_ca_system_score_codex":0.0004189524,"about_ca_system_score_gemma":0.0005093245,"threshold_uncertainty_score":0.23644781},"labels":[],"label_agreement":null},{"id":"W3134982339","doi":"10.1029/2020jb020704","title":"Subducted Lithosphere Under South America From Multifrequency <i>P</i> Wave Tomography","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Engineering and Physical Sciences Research Council; Deutsche Forschungsgemeinschaft","keywords":"Geology; Subduction; Lithosphere; Seismology; Slab; Mantle (geology); Seismic tomography; Oceanic crust; Transition zone; Cretaceous; Paleontology; Geophysics; Tectonics","score_opus":0.05095324108111181,"score_gpt":0.29956878390270947,"score_spread":0.24861554282159765,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3134982339","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9953908,0.000059440492,0.0020824089,0.00012648848,0.0000030725341,0.000005759942,0.0009946163,0.00008853727,0.0012489222],"genre_scores_gemma":[0.9971111,0.00006433885,0.0014040881,0.000012226688,0.000003828986,0.000004656048,0.0011498636,0.000016610717,0.00023338496],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995756,0.0000064839423,0.0000023307311,0.0000142612935,0.0000093208,0.0000100591],"domain_scores_gemma":[0.99990606,0.000014460547,0.000029925513,0.000013642227,0.00002533381,0.0000105281415],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001148061,0.0003245528,0.00011010237,0.00055530126,0.00014605268,0.0005147093,0.00028020216,0.00022376195,0.0013705193],"category_scores_gemma":[0.00046105374,0.00016386328,0.00031400062,0.000947438,0.00019455417,0.00036435865,0.00047850836,0.00021023481,0.00012580353],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021449031,0.000059887843,0.6962168,0.00008928199,0.00024364861,0.0005123331,0.00041721063,0.18831706,0.039500684,0.0022216735,0.0018898791,0.07031693],"study_design_scores_gemma":[0.00007245451,0.000045990502,0.648227,0.000032416396,0.000109109744,0.00024244319,0.0004636483,0.3417137,0.004249534,0.0013050877,0.0035037936,0.000034845176],"about_ca_topic_score_codex":0.051347356,"about_ca_topic_score_gemma":0.05846525,"teacher_disagreement_score":0.051347356,"about_ca_system_score_codex":0.00040685904,"about_ca_system_score_gemma":0.00072683825,"threshold_uncertainty_score":0.102096915},"labels":[],"label_agreement":null},{"id":"W3136486895","doi":"10.1029/2020jb021537","title":"The Viscosity of the Top Third of the Lower Mantle Estimated Using GPS, GRACE, and Relative Sea Level Measurements of Glacial Isostatic Adjustment","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Post-glacial rebound; Geology; Mantle (geology); Ice sheet; Geodesy; Glacial period; Geophysics; Geomorphology","score_opus":0.14033921542647662,"score_gpt":0.3474977287231223,"score_spread":0.20715851329664567,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3136486895","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983152,0.00006966239,0.0003563416,0.000025383635,0.000001596933,0.0000019128486,0.000668809,0.000024155606,0.00053699175],"genre_scores_gemma":[0.99837565,0.00004133361,0.000350605,0.0000054012908,0.0000023243115,0.0000030711094,0.0011039928,0.000008246674,0.00010920208],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999864,0.000020910647,0.0000075428597,0.00004106964,0.000032991793,0.000033438584],"domain_scores_gemma":[0.99971324,0.000043090713,0.00010075567,0.000034630506,0.00005768232,0.000050609677],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036791386,0.00042049424,0.000296401,0.0012472133,0.00027217512,0.0009577729,0.00038776585,0.00024971252,0.00063711806],"category_scores_gemma":[0.0008740915,0.00029520807,0.0007252103,0.00096799486,0.00028414902,0.00061948964,0.0006325003,0.00024296746,0.00018592592],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013484927,0.000021483855,0.9556212,0.000024216255,0.00019032144,0.000091062415,0.00012206793,0.0329261,0.0032362437,0.00026029962,0.00043760176,0.006934548],"study_design_scores_gemma":[0.000020295733,0.000037113743,0.8911553,0.000026214757,0.00007500451,0.00005796518,0.00020037265,0.10487692,0.0022438734,0.00017717497,0.0010917396,0.000038020986],"about_ca_topic_score_codex":0.093607806,"about_ca_topic_score_gemma":0.09859961,"teacher_disagreement_score":0.093607806,"about_ca_system_score_codex":0.0011673588,"about_ca_system_score_gemma":0.0009532578,"threshold_uncertainty_score":0.18612593},"labels":[],"label_agreement":null},{"id":"W3137298505","doi":"10.1029/2021jb022797","title":"The 2019–2020 Khalili (Iran) Earthquake Sequence—Anthropogenic Seismicity in the Zagros Simply Folded Belt?","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ; Natural Sciences and Engineering Research Council of Canada; Deutsche Forschungsgemeinschaft; Iran National Science Foundation; Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; Universidad de Granada; Canada Foundation for Innovation","keywords":"Geology; Induced seismicity; Seismology; Aftershock; Hypocenter; Sequence (biology); Interferometric synthetic aperture radar; Seismic hazard; Synthetic aperture radar","score_opus":0.07053006481328974,"score_gpt":0.3498190958265939,"score_spread":0.27928903101330416,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3137298505","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99956816,0.000027959602,0.00003762577,0.00003744507,0.0000023011853,0.0000014919235,0.000058495367,0.0000024467624,0.0002640298],"genre_scores_gemma":[0.9996674,0.000025296742,0.000052679563,0.000009623075,0.000006028459,0.0000010804723,0.0001580047,7.7023117e-7,0.000079001795],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999298,0.0000064222527,0.0000050064564,0.00001934771,0.000014445425,0.000024972314],"domain_scores_gemma":[0.9998178,0.000011415505,0.0001047538,0.0000120786735,0.000026241352,0.00002771491],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014564104,0.00011860484,0.00011434863,0.0004804465,0.00023858219,0.00038720158,0.00019853524,0.00023627453,0.0008070259],"category_scores_gemma":[0.0002710652,0.000082599334,0.00012254633,0.00057301746,0.00027128236,0.00023944314,0.00020693622,0.00016102692,0.00017651575],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000060195216,0.000026670863,0.9917902,0.0000097425145,0.000019350338,0.0002493966,0.0001736663,0.0004591016,0.001717126,0.0001327844,0.00016845738,0.0051933583],"study_design_scores_gemma":[0.0000021796827,0.000015252241,0.9988287,0.000002409849,0.0000050119156,0.00006299538,0.00022817386,0.00056124397,0.00007999068,0.000023755952,0.00018876558,0.0000015961232],"about_ca_topic_score_codex":0.017201021,"about_ca_topic_score_gemma":0.027414104,"teacher_disagreement_score":0.017201021,"about_ca_system_score_codex":0.0004670034,"about_ca_system_score_gemma":0.0003524218,"threshold_uncertainty_score":0.03420174},"labels":[],"label_agreement":null},{"id":"W3137875871","doi":"10.1029/2021jb021896","title":"Thank You to Our 2020 Peer Reviewers","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Academic Publishing and Open Access","field":"Decision Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Editorial board; Peer review; Psychology; Political science; Library science; Computer science; Law","score_opus":0.20900451367808967,"score_gpt":0.5313825902413942,"score_spread":0.3223780765633045,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3137875871","genre_codex":"editorial","genre_gemma":"editorial","domain_codex":null,"domain_gemma":"evaluation","model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"editorial","genre_consensus":"editorial","domain_candidate":"evaluation","domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00053391105,0.006602423,0.002872322,0.19018061,0.77855647,0.00040057936,0.0014212572,0.0020252198,0.017407186],"genre_scores_gemma":[0.007339479,0.010278518,0.009095027,0.14139625,0.46846092,0.00096051866,0.0027918252,0.0038765497,0.35580087],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9729998,0.0049475026,0.0024356886,0.0032031243,0.015053452,0.0013603687],"domain_scores_gemma":[0.55543894,0.0121287415,0.010730109,0.008967617,0.382221,0.030513544],"candidate_categories":["metaresearch"],"consensus_categories":[],"category_scores_codex":[0.019749,0.0019995053,0.0022820898,0.0046978416,0.004535537,0.01899305,0.0028214615,0.006234038,0.14622344],"category_scores_gemma":[0.1810014,0.0010094008,0.0016397233,0.0026669544,0.0021720137,0.007477562,0.0046708854,0.00844296,0.230505],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012987759,0.000005612376,0.00009813576,0.000057073426,0.000004115911,0.000043157197,0.000032063937,0.000010807156,0.00007259855,0.00013581899,0.98895663,0.010570983],"study_design_scores_gemma":[0.000010947389,0.000008856219,0.00024039301,0.00009365695,0.000008649054,0.00013685678,0.00018883892,0.00004751575,0.00008956586,0.0004937893,0.9986557,0.000025331874],"about_ca_topic_score_codex":0.003595638,"about_ca_topic_score_gemma":0.009190423,"teacher_disagreement_score":0.980251,"about_ca_system_score_codex":0.0022049241,"about_ca_system_score_gemma":0.011359207,"threshold_uncertainty_score":0.48916614},"labels":[],"label_agreement":null},{"id":"W3137982435","doi":"10.1029/2020jb021362","title":"Spatiotemporal Analysis of Seismotectonic State of Injection‐Induced Seismicity Clusters in the Western Canada Sedimentary Basin","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geoscience BC; University of Victoria; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Induced seismicity; Seismology; Geology; Hydraulic fracturing; Magnitude (astronomy); Structural basin; Geotechnical engineering; Geomorphology","score_opus":0.03942951640531647,"score_gpt":0.30536418143706945,"score_spread":0.265934665031753,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3137982435","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99875796,0.000028504743,0.00016070591,0.000018068624,8.11177e-7,0.000006587496,0.0005507039,0.000007971692,0.00046869868],"genre_scores_gemma":[0.9991616,0.000024450152,0.0000942805,0.000002221013,6.357558e-7,0.0000030227761,0.0005130006,0.0000013256697,0.00019956307],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985814,0.000009827465,0.000007018444,0.000028193683,0.000050065868,0.000046777383],"domain_scores_gemma":[0.9993155,0.000060880455,0.00015285535,0.000025949514,0.00031191533,0.00013299265],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014933532,0.00014738848,0.0002015269,0.0016685994,0.0005822473,0.0006174063,0.00034467602,0.00014571994,0.0008310984],"category_scores_gemma":[0.00092522346,0.00012907677,0.00015819875,0.0023527348,0.00045214384,0.00012330213,0.00041484134,0.00017345481,0.00008307788],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019006088,0.000049257036,0.9712436,0.000036141537,0.0001223414,0.00023712566,0.0011019908,0.0063805073,0.0070967753,0.00036187063,0.0007465301,0.012433676],"study_design_scores_gemma":[0.0000018071468,0.0000066492285,0.9959241,0.000003867941,0.000008552945,0.000012486485,0.00035798099,0.0032537102,0.00018254435,0.000017497796,0.0002256617,0.0000051300563],"about_ca_topic_score_codex":0.9307181,"about_ca_topic_score_gemma":0.9481422,"teacher_disagreement_score":0.069281876,"about_ca_system_score_codex":0.0038778032,"about_ca_system_score_gemma":0.0031828862,"threshold_uncertainty_score":0.13937974},"labels":[],"label_agreement":null},{"id":"W3137984631","doi":"10.1029/2020jb020950","title":"Amplification and Tuning of Ground Motion at the Outer Cascadia Accretionary Prism","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Accretionary wedge; Seismology; Prism; Subduction; Seismometer; Ridge; Bedrock; Amplitude; Microseism; Geodesy; Geomorphology; Optics; Tectonics; Paleontology; Physics","score_opus":0.04668231647428137,"score_gpt":0.31331249523820254,"score_spread":0.26663017876392114,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3137984631","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998743,0.000018175158,0.00015116938,0.000008933588,0.0000013610559,0.0000023635607,0.00010210933,0.00002246069,0.0009505286],"genre_scores_gemma":[0.9995901,0.000011581957,0.00006219275,0.0000034320537,0.0000014634815,0.0000018938009,0.00011919156,0.0000025549336,0.00020764692],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998381,0.000016281578,0.000009902625,0.00004886828,0.000049185666,0.000037632053],"domain_scores_gemma":[0.99957126,0.000054179825,0.00011226953,0.00004807126,0.00012419462,0.00009003817],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019384074,0.00028055153,0.00018660384,0.0008181994,0.00022463109,0.0003520915,0.00023651976,0.00016402209,0.0011792043],"category_scores_gemma":[0.0007758788,0.00018449548,0.00015905395,0.0005587323,0.00026238037,0.00013806846,0.00074089563,0.00018744232,0.00019342385],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005874347,0.000040028975,0.7474691,0.000069775364,0.0001207214,0.00079529005,0.0011991943,0.0020389855,0.22656254,0.00009781671,0.00026634333,0.020752778],"study_design_scores_gemma":[0.0000016661763,0.000018515402,0.9985251,0.0000018738274,0.0000045301913,0.00004197563,0.00006947068,0.00034038496,0.0008467024,0.000008307082,0.00013909017,0.0000025200993],"about_ca_topic_score_codex":0.013407539,"about_ca_topic_score_gemma":0.013930346,"teacher_disagreement_score":0.013407539,"about_ca_system_score_codex":0.00041141408,"about_ca_system_score_gemma":0.00016561076,"threshold_uncertainty_score":0.026658952},"labels":[],"label_agreement":null},{"id":"W3138504939","doi":"10.1029/2020jb021434","title":"Stacked Magma Lenses Beneath Mid‐Ocean Ridges: Insights From New Seismic Observations and Synthesis With Prior Geophysical and Geologic Findings","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Lamont-Doherty Earth Observatory, Columbia University; Woods Hole Oceanographic Institution; National Science Foundation","keywords":"Geology; Sill; Crust; Magma; Ridge; Mid-ocean ridge; Magma chamber; Seamount; Oceanic crust; Seismology; Lava; Petrology; Volcano; Geophysics; Tectonics; Subduction; Geochemistry; Paleontology","score_opus":0.044564532391925406,"score_gpt":0.26209674879957734,"score_spread":0.21753221640765194,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3138504939","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99673235,0.00042384714,0.0007564552,0.00003116648,0.000010273087,0.000007737616,0.00030087424,0.00007224033,0.0016650428],"genre_scores_gemma":[0.9984706,0.00017647084,0.00093111757,0.000007151084,0.000012706529,0.0000017151083,0.00024297391,0.000008956033,0.00014833416],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999007,0.0000050643,0.000008685609,0.000032277967,0.000031797947,0.000021468322],"domain_scores_gemma":[0.99975365,0.000022079144,0.000094332136,0.000038006845,0.00006440842,0.000027569493],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020582364,0.00026406886,0.00019049266,0.0010725076,0.0001825465,0.0006809001,0.00027911883,0.00023558554,0.00092443],"category_scores_gemma":[0.0004377469,0.00022445875,0.00036174708,0.0008094835,0.00025715033,0.0003014817,0.0004634678,0.00018304515,0.00012740286],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015099453,0.00007538578,0.8275539,0.00023625226,0.0002424384,0.00061873073,0.0011693725,0.0021872,0.11848187,0.00021470516,0.00028115985,0.048788045],"study_design_scores_gemma":[0.0000032390872,0.000019555686,0.99455583,0.00001450031,0.000049168102,0.00014774456,0.00029098164,0.0018806583,0.0022060953,0.000038252918,0.0007870754,0.000006957531],"about_ca_topic_score_codex":0.0075165266,"about_ca_topic_score_gemma":0.0188158,"teacher_disagreement_score":0.0075165266,"about_ca_system_score_codex":0.00026414188,"about_ca_system_score_gemma":0.0002460315,"threshold_uncertainty_score":0.014945567},"labels":[],"label_agreement":null},{"id":"W3139395088","doi":"10.1029/2020jb021196","title":"The Role of Fluid Pressure‐Induced Aseismic Slip in Earthquake Cycle Modulation","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Hudbay Minerals (Canada); Earthgen; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Government of Ontario; University of Toronto; University of Michigan","keywords":"Induced seismicity; Seismology; Geology; Slip (aerodynamics); Perturbation (astronomy); Pore water pressure; Fluid pressure; Seismic hazard; Mechanics; Geotechnical engineering; Engineering; Physics","score_opus":0.029767459126492545,"score_gpt":0.30267881408545033,"score_spread":0.2729113549589578,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3139395088","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9957521,0.00010992639,0.0030142434,0.00005262719,0.0000049740415,0.0000060879743,0.000051385734,0.000026676318,0.0009820476],"genre_scores_gemma":[0.9998344,0.000022623539,0.00009804657,0.0000015337041,8.1307724e-7,0.0000013103063,0.000006003395,0.0000010534351,0.000034109904],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999461,0.000014760051,0.0000043793502,0.000011201207,0.000010492257,0.000013049299],"domain_scores_gemma":[0.9997004,0.00012725402,0.00009017063,0.000022066097,0.000024808443,0.000035251636],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001446512,0.00017828116,0.00019225609,0.00022543375,0.00015143029,0.0004922774,0.000240037,0.00028697908,0.00073830225],"category_scores_gemma":[0.0009853547,0.00012494755,0.0001574256,0.00014577845,0.0003949834,0.00038733392,0.0003373261,0.00018219855,0.00007348419],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00059988187,0.000274017,0.08546816,0.00015747274,0.0000968829,0.00092477165,0.00022209215,0.57554656,0.31223926,0.005425157,0.00029675072,0.018749107],"study_design_scores_gemma":[0.000016744512,0.00016651444,0.055745985,0.000009163676,0.000022991233,0.000096007076,0.00008321352,0.9295898,0.012746618,0.0011441428,0.000360115,0.000018688283],"about_ca_topic_score_codex":0.0018678743,"about_ca_topic_score_gemma":0.00087790226,"teacher_disagreement_score":0.0018678743,"about_ca_system_score_codex":0.00030761078,"about_ca_system_score_gemma":0.00029293544,"threshold_uncertainty_score":0.003714025},"labels":[],"label_agreement":null},{"id":"W3145328124","doi":"10.1029/2020jb020998","title":"Analysis of Crystalline Rock Permeability Versus Depth in a Canadian Precambrian Rock Setting","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Groundwater flow and contamination studies","field":"Environmental Science","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Waterloo","funders":"Nuclear Waste Management Organization","keywords":"Precambrian; Geology; Lithology; Pluton; Permeability (electromagnetism); Geochemistry; Shield; Petrology; Seismology; Chemistry","score_opus":0.03403338160856648,"score_gpt":0.3319420745983385,"score_spread":0.297908692989772,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3145328124","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99669564,0.00017194914,0.0006845182,0.000012718983,7.3078166e-7,0.000022601933,0.0008450536,0.000032427903,0.0015343261],"genre_scores_gemma":[0.998638,0.0000985629,0.00069399143,0.0000032330538,4.2963697e-7,0.000006297209,0.00032878466,0.0000041123762,0.00022654372],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997218,0.000009551841,0.000008889889,0.00004655233,0.00013483063,0.00007838296],"domain_scores_gemma":[0.99938536,0.00009567043,0.000087502325,0.000025754602,0.00035304792,0.000052789812],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002580116,0.00032623293,0.00023589122,0.0034236964,0.0010638087,0.0007273139,0.0004664815,0.00023603225,0.0008214317],"category_scores_gemma":[0.0010592716,0.00019404323,0.0002921645,0.0032239964,0.00071712397,0.0002673913,0.00057939603,0.0002162622,0.00009546625],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00057608803,0.00006698673,0.7997974,0.00023098382,0.00017097002,0.0007005724,0.0021492457,0.017292859,0.117430255,0.0015598749,0.0005411402,0.059483636],"study_design_scores_gemma":[0.000006155322,0.000035601126,0.97407055,0.000012094573,0.00004638013,0.0001629566,0.00091171433,0.0095665185,0.013799968,0.00014264222,0.001215964,0.000029322411],"about_ca_topic_score_codex":0.9370693,"about_ca_topic_score_gemma":0.960082,"teacher_disagreement_score":0.0629307,"about_ca_system_score_codex":0.0060926513,"about_ca_system_score_gemma":0.004588451,"threshold_uncertainty_score":0.12660259},"labels":[],"label_agreement":null},{"id":"W3148823046","doi":"10.1029/2020jb019781","title":"Thank You to Our 2019 Reviewers","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Academic Publishing and Open Access","field":"Decision Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Point (geometry); Key (lock); Computer science; Library science; Information retrieval; Mathematics; Computer security; Geometry","score_opus":0.26890631059455083,"score_gpt":0.5259212716089434,"score_spread":0.2570149610143926,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3148823046","genre_codex":"editorial","genre_gemma":"editorial","domain_codex":null,"domain_gemma":"evaluation","model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"editorial","genre_consensus":"editorial","domain_candidate":"evaluation","domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0003798211,0.0064658695,0.0014446821,0.22942275,0.74874943,0.00031049686,0.001633134,0.0010326026,0.010561278],"genre_scores_gemma":[0.008350984,0.0060997847,0.005225968,0.17476134,0.43185455,0.0008015523,0.0018076055,0.0027456388,0.36835253],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9836866,0.003139604,0.001943112,0.0023233772,0.007965832,0.0009415077],"domain_scores_gemma":[0.56880695,0.010233233,0.0132351555,0.005503688,0.37580281,0.026418213],"candidate_categories":["metaresearch"],"consensus_categories":[],"category_scores_codex":[0.015871616,0.0019746677,0.002283078,0.0059325537,0.0038268168,0.014924138,0.002284349,0.0059969607,0.13125521],"category_scores_gemma":[0.15435167,0.0007996316,0.0017437264,0.0024448272,0.001688531,0.005756359,0.0044337083,0.0071628764,0.14752807],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016719487,0.0000029745577,0.00011800635,0.000063900145,0.000005503242,0.000065308406,0.000039111925,0.0000074111294,0.00007212207,0.00014834649,0.99492514,0.0045355074],"study_design_scores_gemma":[0.00001465931,0.00000984664,0.00035293752,0.00015302635,0.000013561099,0.00020760675,0.00036172033,0.00004329684,0.0000971657,0.0005194253,0.9981927,0.000033953304],"about_ca_topic_score_codex":0.0053354637,"about_ca_topic_score_gemma":0.015149776,"teacher_disagreement_score":0.98412836,"about_ca_system_score_codex":0.003577223,"about_ca_system_score_gemma":0.007714003,"threshold_uncertainty_score":0.4390924},"labels":[],"label_agreement":null},{"id":"W3151319682","doi":"10.1029/2020jb021221","title":"States of In Situ Stress in the Duvernay East Shale Basin and Willesden Green of Alberta, Canada: Variable In Situ Stress States Effect Fault Stability","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Alberta Energy; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; University of Alberta; Purdue University","keywords":"Induced seismicity; Geology; Hydraulic fracturing; Borehole; Seismology; Pore water pressure; Fault (geology); Slip (aerodynamics); Microseism; Fault plane; Structural basin; Stress field; Differential stress; Petrology; Shear (geology); Geotechnical engineering; Deformation (meteorology); Geomorphology; Engineering","score_opus":0.019004179338103538,"score_gpt":0.26894933578912705,"score_spread":0.24994515645102353,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3151319682","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993892,0.000013768996,0.000037327667,0.00001275843,5.047698e-7,0.0000029922867,0.00018369922,0.000003881235,0.0003559595],"genre_scores_gemma":[0.99953854,0.000015169686,0.000054236265,0.0000046687765,3.0547199e-7,0.0000015393334,0.00016547556,0.0000011495326,0.00021883828],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998197,0.000019558709,0.000008807667,0.000034597877,0.00005303336,0.000064326065],"domain_scores_gemma":[0.99946743,0.00009724897,0.000065479806,0.000024427307,0.00024032332,0.00010506581],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027443792,0.00025945442,0.00023768014,0.0008349431,0.0008532367,0.0010383595,0.0005696665,0.00027183097,0.000761815],"category_scores_gemma":[0.0011111939,0.00018558392,0.00014813805,0.0013099506,0.0008727646,0.00021802951,0.00044341135,0.00016273238,0.00006312232],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031378563,0.00009640345,0.97051406,0.000030573046,0.00009643453,0.00024609265,0.0011724973,0.010920443,0.0075168284,0.00035468076,0.0003850376,0.008353273],"study_design_scores_gemma":[0.000006524903,0.000013977885,0.9926247,0.0000050561916,0.000012025628,0.000013269305,0.0009467549,0.005580644,0.0005419109,0.000043086875,0.00020325866,0.000008801863],"about_ca_topic_score_codex":0.97317797,"about_ca_topic_score_gemma":0.98769057,"teacher_disagreement_score":0.02682203,"about_ca_system_score_codex":0.008973828,"about_ca_system_score_gemma":0.006007416,"threshold_uncertainty_score":0.06510997},"labels":[],"label_agreement":null},{"id":"W3157495107","doi":"10.1029/2021jb022258","title":"Characterization of Irreversible Land Subsidence in the Yazd‐Ardakan Plain, Iran From 2003 to 2020 InSAR Time Series","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Synthetic Aperture Radar (SAR) Applications and Techniques","field":"Engineering","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Chinese Academy of Sciences; National Natural Science Foundation of China; National Aeronautics and Space Administration","keywords":"Interferometric synthetic aperture radar; Aquifer; Subsidence; Groundwater; Geology; Groundwater recharge; Land reclamation; Groundwater-related subsidence; Hydrology (agriculture); Geomorphology; Geotechnical engineering; Synthetic aperture radar; Geography; Remote sensing; Structural basin","score_opus":0.0185945200795277,"score_gpt":0.28449938775976685,"score_spread":0.26590486768023913,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3157495107","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997757,0.00003950559,0.00032894575,0.00003286568,0.0000034224684,0.000004969609,0.0013276334,0.0000202546,0.00048528108],"genre_scores_gemma":[0.9970642,0.00004222656,0.00023332902,0.0000057533334,0.000003840365,0.0000055098903,0.002473814,0.0000021459493,0.00016920564],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985707,0.000012212421,0.0000124277585,0.000029018127,0.00005631054,0.000033040276],"domain_scores_gemma":[0.99956757,0.00005322613,0.00016513717,0.00003219983,0.00015322425,0.00002860923],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003653576,0.00025049705,0.00015086345,0.001273731,0.00015671585,0.00037801088,0.00021624882,0.00017726835,0.00045336716],"category_scores_gemma":[0.000693434,0.00007931453,0.00021447896,0.0015465548,0.00017431864,0.00023275806,0.00018189772,0.00017585035,0.000195166],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012333615,0.00007327782,0.96483797,0.000020734245,0.000052269854,0.00024085765,0.00014311502,0.01131028,0.00223039,0.000257137,0.0011379268,0.019572861],"study_design_scores_gemma":[0.0000023515474,0.000021812537,0.9902564,0.0000024153155,0.000008722707,0.000039304043,0.00014119725,0.00852317,0.00037605627,0.00003850632,0.00058611715,0.0000040162827],"about_ca_topic_score_codex":0.028788706,"about_ca_topic_score_gemma":0.031362057,"teacher_disagreement_score":0.028788706,"about_ca_system_score_codex":0.000518387,"about_ca_system_score_gemma":0.0004018578,"threshold_uncertainty_score":0.057242274},"labels":[],"label_agreement":null},{"id":"W3157858215","doi":"10.1029/2020jb020308","title":"Investigation on Two M<sub>w</sub> 3.6 and M<sub>w</sub> 4.1 Earthquakes Triggered by Poroelastic Effects of Hydraulic Fracturing Operations Near Crooked Lake, Alberta","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Virtual Materials Group (Canada); University of Calgary","funders":"Canada First Research Excellence Fund","keywords":"Poromechanics; Geology; Hydraulic fracturing; Pore water pressure; Geomechanics; Fault (geology); Seismology; Induced seismicity; Slip (aerodynamics); Fluid pressure; Permeability (electromagnetism); Effective stress; Geotechnical engineering; Petrology; Mechanics; Engineering","score_opus":0.024705724865276724,"score_gpt":0.272006113906878,"score_spread":0.2473003890416013,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3157858215","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993457,0.000008231064,0.00014962617,0.00001051166,0.0000011932663,0.0000069458024,0.00005279486,0.0000100105535,0.00041497475],"genre_scores_gemma":[0.9994172,0.000014205589,0.00020226993,0.0000048405377,6.12368e-7,0.000002820215,0.00005673582,0.0000018429114,0.00029948945],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99995375,0.0000023881723,0.0000013814843,0.000006052402,0.000020539592,0.00001587022],"domain_scores_gemma":[0.9999397,0.00000819073,0.000010712229,0.000004105252,0.000019226338,0.000018059993],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006155209,0.00019104619,0.00017562295,0.00028844745,0.0005110998,0.00024247475,0.00029831319,0.00030652087,0.00064432825],"category_scores_gemma":[0.000090252244,0.00011528308,0.00018295548,0.00024251245,0.0002660514,0.000109302855,0.000172913,0.00021070919,0.00006343411],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011150348,0.0005982832,0.35057828,0.00018231022,0.00010184106,0.004023573,0.00089013536,0.061955072,0.5554266,0.0007475061,0.0007059469,0.023675393],"study_design_scores_gemma":[0.000037555088,0.00031776985,0.9047003,0.000005932984,0.000043627653,0.00012739738,0.0012451971,0.06404579,0.028541071,0.000086883425,0.00082406605,0.000024395462],"about_ca_topic_score_codex":0.21479154,"about_ca_topic_score_gemma":0.37551042,"teacher_disagreement_score":0.78520846,"about_ca_system_score_codex":0.0012801497,"about_ca_system_score_gemma":0.0007946505,"threshold_uncertainty_score":0.4270826},"labels":[],"label_agreement":null},{"id":"W3157941603","doi":"10.1029/2021jb022351","title":"Plain Language Summary Required for Submission to <i>Journal of Geophysical Research: Solid Earth</i>","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Marine and environmental studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Solid earth; Earth (classical element); Geophysics; Earth science; Astrobiology; Geology; Library science; Computer science; Physics; Astronomy","score_opus":0.07422455747043888,"score_gpt":0.36067186957740144,"score_spread":0.28644731210696256,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3157941603","genre_codex":"editorial","genre_gemma":"editorial","domain_codex":null,"domain_gemma":"reporting","model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"editorial","genre_consensus":"editorial","domain_candidate":"reporting","domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0013046992,0.0018046475,0.011578649,0.069476865,0.37101167,0.007674446,0.16469996,0.026868535,0.34558055],"genre_scores_gemma":[0.005523833,0.002603783,0.009617667,0.022029467,0.07816286,0.0061094468,0.08877365,0.020024486,0.76715493],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9931664,0.0012036839,0.0017896567,0.0006112307,0.0026459754,0.0005830043],"domain_scores_gemma":[0.88953465,0.016952723,0.009412478,0.0070394585,0.067677796,0.009382897],"candidate_categories":["metaresearch","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.008549842,0.0019555422,0.0027816894,0.005964251,0.0032312293,0.017765548,0.0026488022,0.0045382506,0.65982264],"category_scores_gemma":[0.08861114,0.0017460653,0.0018192763,0.004909455,0.0013633794,0.0054466063,0.0029318319,0.0059327874,0.70685416],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004851492,0.00001303246,0.000024740675,0.00016252922,0.0000035785404,0.00002635038,0.000014201833,0.000024427265,0.0003082163,0.00027644646,0.99586064,0.0032373513],"study_design_scores_gemma":[0.000084382445,0.00006687141,0.0005754218,0.00017563715,0.000007695668,0.000039903374,0.00006854358,0.000076149256,0.00035492706,0.0007091721,0.9978067,0.00003453227],"about_ca_topic_score_codex":0.0029784925,"about_ca_topic_score_gemma":0.0030664983,"teacher_disagreement_score":0.99145013,"about_ca_system_score_codex":0.0023061081,"about_ca_system_score_gemma":0.0070001814,"threshold_uncertainty_score":0.48522168},"labels":[],"label_agreement":null},{"id":"W3158704335","doi":"10.1029/2020jb021511","title":"Pore Habit of Gas in Gassy Sediments","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Sediment; Classification of discontinuities; Habit; Mineralogy; Nucleation; Petroleum engineering; Geotechnical engineering; Geochemistry; Geomorphology; Chemistry","score_opus":0.029664111811213666,"score_gpt":0.3312202055485779,"score_spread":0.30155609373736425,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3158704335","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994677,0.000010424208,0.00026398033,0.0000028174004,3.8744594e-7,0.0000018421839,0.000076912685,0.000017318322,0.00015873593],"genre_scores_gemma":[0.99981195,0.0000055330893,0.000093274946,6.6908547e-7,1.722562e-7,9.1197506e-7,0.00003244323,0.0000013445983,0.000053726853],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999279,0.000004952161,0.000004210049,0.000028905251,0.000016832057,0.000017239747],"domain_scores_gemma":[0.9998031,0.00006158838,0.00005381561,0.000017808792,0.000039216033,0.000024470728],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000100033954,0.00018022157,0.00013651168,0.00055651146,0.00023971633,0.00039889754,0.00023332977,0.00026082573,0.0008920931],"category_scores_gemma":[0.00037409275,0.00013316442,0.00009213901,0.00032537847,0.0004976122,0.00023671717,0.00026385268,0.00015048387,0.000056649205],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006420581,0.00008203051,0.20726329,0.00012795674,0.00003746708,0.0006173868,0.00046936897,0.027738828,0.75312346,0.0004891167,0.00009898486,0.009309957],"study_design_scores_gemma":[0.000020766463,0.0002540325,0.71259487,0.000014634837,0.000026146932,0.00017757867,0.00060471013,0.09760372,0.1879012,0.00026486383,0.0005022868,0.000035150602],"about_ca_topic_score_codex":0.020319642,"about_ca_topic_score_gemma":0.0179435,"teacher_disagreement_score":0.020319642,"about_ca_system_score_codex":0.00037603895,"about_ca_system_score_gemma":0.00014109846,"threshold_uncertainty_score":0.04040271},"labels":[],"label_agreement":null},{"id":"W3159347950","doi":"10.1029/2021jb022358","title":"Distributed Acoustic Sensing in Volcano‐Glacial Environments—Mount Meager, British Columbia","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":85,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Natural Resources Canada; Government of Canada","keywords":"Induced seismicity; Geology; Seismology; Volcano; Seismometer; Mount; Geothermal gradient; Volcanology; Seismic noise; Geophysics; Computer science","score_opus":0.02115783574065141,"score_gpt":0.27388915514210144,"score_spread":0.25273131940145005,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3159347950","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9940779,0.00010852388,0.0007380926,0.00014437437,0.000005385215,0.000020240415,0.00097290246,0.00006040304,0.0038722684],"genre_scores_gemma":[0.99710363,0.000053438886,0.0013658344,0.000021878152,0.000003387913,0.000008783958,0.00038611473,0.0000061448245,0.001050816],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998161,0.000016397682,0.0000046456066,0.000041680556,0.00006969224,0.00005149734],"domain_scores_gemma":[0.99970406,0.00005303092,0.000030472269,0.000025991436,0.000138611,0.00004780739],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016595378,0.00030960323,0.00017974277,0.00067525695,0.0008004199,0.0007232564,0.00058470893,0.00029708707,0.00095790514],"category_scores_gemma":[0.0006430681,0.000107656284,0.00008367833,0.0011947067,0.0003753207,0.00019613028,0.00041717337,0.00029185603,0.00013006444],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044558654,0.00024638398,0.71509916,0.000157701,0.00015041808,0.0020209826,0.0021289962,0.06992725,0.059094585,0.001052025,0.007265532,0.14241138],"study_design_scores_gemma":[0.00004240033,0.000060660645,0.8758375,0.000052311203,0.00003353528,0.00023145172,0.0027571525,0.11039487,0.0044540516,0.00030505323,0.0057716416,0.000059431684],"about_ca_topic_score_codex":0.91217357,"about_ca_topic_score_gemma":0.9725496,"teacher_disagreement_score":0.08782643,"about_ca_system_score_codex":0.0037185117,"about_ca_system_score_gemma":0.0026183035,"threshold_uncertainty_score":0.17668724},"labels":[],"label_agreement":null},{"id":"W3161307582","doi":"10.1029/2020jb021422","title":"Trace Elemental Partitioning on Clays Derived From Hydrothermal Muds of the El Tatio Geyser Field, Chile","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"H2020 European Research Council; Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Kaolinite; Illite; Montmorillonite; Clay minerals; Weathering; Aqueous solution; Chemistry; Leaching (pedology); Environmental chemistry; Geology; Mineralogy; Geochemistry; Soil water; Soil science","score_opus":0.026838866227858603,"score_gpt":0.3006014725811358,"score_spread":0.2737626063532772,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3161307582","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987233,0.00008473984,0.00010417514,0.000014100293,0.0000011766375,0.000012392517,0.00040511347,0.0000067322544,0.0006480932],"genre_scores_gemma":[0.99787915,0.0001106753,0.00040018736,0.000032807162,0.0000028682712,0.000024711817,0.0006139258,0.000008163646,0.0009275416],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999126,0.000004540235,0.0000054324155,0.000032675598,0.000020650225,0.000024103174],"domain_scores_gemma":[0.99989307,0.000016595382,0.000022850643,0.0000046790506,0.000040681247,0.00002213713],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000106250394,0.00031290296,0.00025141943,0.0011239594,0.00051870086,0.0005624898,0.00031919903,0.00022257949,0.00077914185],"category_scores_gemma":[0.00019523785,0.00017640639,0.00015080161,0.0005714423,0.00032540728,0.0002527495,0.00044017704,0.00021505765,0.00014542136],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037190714,0.000095618365,0.21004947,0.00026704324,0.00009921501,0.0009580586,0.0017089604,0.0007720671,0.7755164,0.000092635324,0.00024504296,0.009823603],"study_design_scores_gemma":[0.000035150257,0.00012795962,0.9570317,0.000038020626,0.000037976995,0.00022679448,0.0024628723,0.0011668196,0.036495652,0.000059944818,0.00229598,0.0000210561],"about_ca_topic_score_codex":0.04099048,"about_ca_topic_score_gemma":0.054566525,"teacher_disagreement_score":0.04099048,"about_ca_system_score_codex":0.0006645857,"about_ca_system_score_gemma":0.00043400427,"threshold_uncertainty_score":0.08150375},"labels":[],"label_agreement":null},{"id":"W3162847895","doi":"10.1029/2020jb019981","title":"New Megathrust Locking Model for the Southern Kurile Subduction Zone Incorporating Viscoelastic Relaxation and Non‐Uniform Compliance of Upper Plate","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Subduction; Seismology; Trench; Slip (aerodynamics); Seafloor spreading; Viscoelasticity; Episodic tremor and slip; Tsunami earthquake; Inversion (geology); Geodesy; Geophysics; Tectonics","score_opus":0.07066298588093715,"score_gpt":0.3186622890355948,"score_spread":0.24799930315465762,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3162847895","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5538296,0.00037795852,0.4379719,0.000229781,0.000047657017,0.000056038458,0.00027992908,0.0004197241,0.006787428],"genre_scores_gemma":[0.98873746,0.00011683284,0.008408051,0.000030576008,0.000011785044,0.00005144286,0.00011087672,0.000042691132,0.0024902883],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999925,0.000013072677,0.0000060638527,0.000022499713,0.000017378508,0.00001597911],"domain_scores_gemma":[0.9998838,0.000021183316,0.000037290796,0.000016514396,0.000021826168,0.000019432842],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023082847,0.00049574405,0.0004593703,0.00042007616,0.00023996813,0.00064132566,0.0015521211,0.00073197996,0.0011974279],"category_scores_gemma":[0.00031792498,0.00036678603,0.00083308225,0.00021523469,0.00040374705,0.0007490663,0.00055239286,0.00043312937,0.00024192424],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000025689746,0.000019682813,0.0027248631,0.000013820026,0.000030981482,0.000114192386,0.000038286373,0.9847794,0.00579903,0.0034516808,0.00012971768,0.0028726119],"study_design_scores_gemma":[0.00000442625,0.000007000036,0.00023204558,0.0000018895764,0.000004153281,0.000012110387,0.0000035937694,0.99898905,0.00021335045,0.0004151607,0.00011449292,0.0000026910186],"about_ca_topic_score_codex":0.007084357,"about_ca_topic_score_gemma":0.0045979014,"teacher_disagreement_score":0.007084357,"about_ca_system_score_codex":0.0005421646,"about_ca_system_score_gemma":0.000513209,"threshold_uncertainty_score":0.0140862465},"labels":[],"label_agreement":null},{"id":"W3165483764","doi":"10.1029/2020jb020713","title":"Assessing Global Present‐Day Surface Mass Transport and Glacial Isostatic Adjustment From Inversion of Geodetic Observations","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ocean Networks Canada Society; University of Victoria; Geological Survey of Canada; Natural Resources Canada","funders":"Jet Propulsion Laboratory","keywords":"Post-glacial rebound; Geodetic datum; Geology; Geodesy; Inversion (geology); Glacial period; Geophysics; Geomorphology","score_opus":0.09466153334084783,"score_gpt":0.33683660322339903,"score_spread":0.24217506988255122,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3165483764","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99214435,0.000048701306,0.0064417436,0.00004939437,0.00000843917,0.00000943964,0.00042010506,0.00015703503,0.0007208568],"genre_scores_gemma":[0.99612314,0.000017204757,0.0031189092,0.000010194735,0.0000057230654,0.0000037766306,0.00061098824,0.000013312694,0.00009672634],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986136,0.000030455154,0.000008191704,0.00003615784,0.00003769996,0.000026146794],"domain_scores_gemma":[0.99971527,0.000056649573,0.0000726786,0.00004693289,0.00007484164,0.000033613855],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006677197,0.00044588733,0.00023294186,0.00081693806,0.0001823082,0.00045822572,0.00026937563,0.0003510527,0.00042643727],"category_scores_gemma":[0.0013475958,0.00021151981,0.00046046588,0.0007476948,0.00028721587,0.0004862211,0.00041546507,0.00030981968,0.00015005702],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030143568,0.00020363758,0.60899556,0.00005710647,0.0004257643,0.00016100226,0.00016283766,0.2802476,0.038753778,0.0008225164,0.0009038259,0.068964876],"study_design_scores_gemma":[0.000039511135,0.00008603286,0.41530374,0.000013938878,0.000073832576,0.000044231725,0.0001046608,0.5756639,0.007308903,0.00045385427,0.0008613125,0.000046085046],"about_ca_topic_score_codex":0.024924492,"about_ca_topic_score_gemma":0.028048964,"teacher_disagreement_score":0.024924492,"about_ca_system_score_codex":0.0004892323,"about_ca_system_score_gemma":0.0006080267,"threshold_uncertainty_score":0.04955882},"labels":[],"label_agreement":null},{"id":"W3165550840","doi":"10.1029/2021jb022228","title":"Magnetic and Gravity Surface Geometry Inverse Modeling of the TAG Active Mound","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Mount Allison University; Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada; Memorial University of Newfoundland; Natural Environment Research Council; Sight Research UK","keywords":"Geology; Seafloor spreading; Ridge; Hydrothermal circulation; Magnetic anomaly; Basalt; Geophysics; Drilling; Volcanogenic massive sulfide ore deposit; Geochemistry; Seismology; Paleontology","score_opus":0.04938861785830468,"score_gpt":0.3278297245033159,"score_spread":0.2784411066450112,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3165550840","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95881575,0.000018216293,0.037346836,0.00008976881,0.0000095179275,0.000015008413,0.0003529311,0.0004644475,0.0028876953],"genre_scores_gemma":[0.99286413,0.000008847637,0.006379525,0.0000064588867,0.0000017524444,0.000007389996,0.00016855185,0.000022775472,0.0005405379],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999602,0.000006599566,0.0000016838146,0.000011293051,0.000013710123,0.000006549569],"domain_scores_gemma":[0.9999373,0.000019420118,0.000008152796,0.000010127951,0.000018093737,0.000006880838],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000901051,0.00029380026,0.00019410763,0.0002691166,0.00017033727,0.00037521747,0.00034737942,0.0002888393,0.0006898179],"category_scores_gemma":[0.00026350172,0.0001865768,0.00041839026,0.00018256076,0.00019300473,0.00014010661,0.00018896819,0.0002221169,0.00015960849],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000048503265,0.00004374844,0.011866197,0.000016381293,0.000023228331,0.00012574374,0.000074671974,0.9602633,0.01672754,0.00051758334,0.00026021877,0.010032769],"study_design_scores_gemma":[0.000003927495,0.0000063478597,0.002751708,6.28214e-7,0.0000020738723,0.000010068655,0.000011017926,0.9961747,0.00082644226,0.000076987795,0.00013250021,0.0000035844346],"about_ca_topic_score_codex":0.028404485,"about_ca_topic_score_gemma":0.020668717,"teacher_disagreement_score":0.028404485,"about_ca_system_score_codex":0.00034887323,"about_ca_system_score_gemma":0.0006391774,"threshold_uncertainty_score":0.056478262},"labels":[],"label_agreement":null},{"id":"W3169934237","doi":"10.1029/2021jb021648","title":"Adjoint Tomography of Ambient Noise Data and Teleseismic P Waves: Methodology and Applications to Central California","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Australian Research Council; Natural Sciences and Engineering Research Council of Canada; University of Toronto; Canada Foundation for Innovation","keywords":"Classification of discontinuities; Geology; Inversion (geology); Ambient noise level; Tomography; Lithosphere; Seismic tomography; Seismology; Geophysics; Noise (video); Earth structure; Geodesy; Mantle (geology); Physics; Computer science; Tectonics; Optics; Mathematics; Mathematical analysis","score_opus":0.09641415950762433,"score_gpt":0.3633684554193171,"score_spread":0.2669542959116928,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3169934237","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9497924,0.0000586756,0.048271045,0.000054898817,0.0000073160872,0.000022898463,0.00011898847,0.00034328323,0.0013304546],"genre_scores_gemma":[0.9761429,0.000019797715,0.02333895,0.000009086904,0.0000044845983,0.000011003138,0.00011767961,0.000017947737,0.00033801864],"study_design_codex":"simulation_or_modeling","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998468,0.000023982224,0.00000995627,0.00005907647,0.000040605762,0.000019495328],"domain_scores_gemma":[0.9997311,0.00007989095,0.000037874786,0.000033945427,0.00009485504,0.00002226854],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00046027277,0.00035887345,0.00023759494,0.0005960469,0.00032702045,0.00059193204,0.000551128,0.00026151226,0.0003702198],"category_scores_gemma":[0.0012873062,0.00025316456,0.00022543698,0.00073326955,0.00037784013,0.00029499707,0.0005835646,0.0003407365,0.000032010674],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033283388,0.00021193354,0.10170579,0.000069989714,0.00012931894,0.0005302325,0.0005044734,0.68647265,0.022098234,0.004332093,0.000670338,0.18294212],"study_design_scores_gemma":[0.00005272899,0.000032140713,0.02171223,0.000010004462,0.000027829823,0.000039560568,0.0001570514,0.9736733,0.0029044747,0.0008839856,0.00048325575,0.000023396875],"about_ca_topic_score_codex":0.1320897,"about_ca_topic_score_gemma":0.119079314,"teacher_disagreement_score":0.1320897,"about_ca_system_score_codex":0.00051423436,"about_ca_system_score_gemma":0.0012571154,"threshold_uncertainty_score":0.26264173},"labels":[],"label_agreement":null},{"id":"W3170754246","doi":"10.1029/2021jb021963","title":"A Granular Jamming Model for Low‐Frequency Earthquakes","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"Japan Society for the Promotion of Science; Natural Sciences and Engineering Research Council of Canada","keywords":"Slip (aerodynamics); Jamming; Seismology; Seismic moment; Geology; Granular material; Context (archaeology); Physics; Mechanics; Geotechnical engineering; Condensed matter physics; Fault (geology)","score_opus":0.06489501007304425,"score_gpt":0.33444373737440697,"score_spread":0.2695487273013627,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3170754246","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.88440967,0.00039352453,0.10068691,0.0008281161,0.00007802825,0.00008955927,0.0009397299,0.0004334326,0.012140961],"genre_scores_gemma":[0.9956428,0.00011014885,0.0015570222,0.00002288587,0.000023628203,0.000022565291,0.00017646764,0.000023969644,0.0024205702],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998105,0.0000401832,0.000008967709,0.00003925861,0.000039591956,0.00006158519],"domain_scores_gemma":[0.99917287,0.0002847236,0.0002303239,0.000053634172,0.000105376166,0.00015298257],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000630747,0.00043108012,0.0006093738,0.0014568515,0.0008105773,0.0019300671,0.0013133379,0.0010047881,0.0033559978],"category_scores_gemma":[0.0026556018,0.00031312768,0.00059537153,0.00082245807,0.000975482,0.0011308048,0.0007562739,0.0006952159,0.00045818862],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015404022,0.00011431478,0.020051168,0.00004364768,0.00005983714,0.00056246755,0.00019616494,0.91098,0.0017245122,0.058415134,0.0019205784,0.005778195],"study_design_scores_gemma":[0.00000873036,0.000007785898,0.0010422833,0.0000030635867,0.0000056964586,0.000020712438,0.00001841953,0.99471223,0.000023284445,0.00399889,0.00015485399,0.000004106611],"about_ca_topic_score_codex":0.0424557,"about_ca_topic_score_gemma":0.019746827,"teacher_disagreement_score":0.0424557,"about_ca_system_score_codex":0.0014589243,"about_ca_system_score_gemma":0.00079730793,"threshold_uncertainty_score":0.084417164},"labels":[],"label_agreement":null},{"id":"W3174971506","doi":"10.1029/2021jb021784","title":"Numerical Modeling of Complex Stress State in a Fault Damage Zone and Its Implication on Near‐Fault Seismic Activity","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Rock Mechanics and Modeling","field":"Engineering","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Japan Society for the Promotion of Science","keywords":"Geology; Seismology; Induced seismicity; Rock mass classification; Fault (geology); Parametric statistics; Fracture (geology); Stress (linguistics); Geotechnical engineering; Cauchy stress tensor; Structural engineering; Engineering; Mathematics","score_opus":0.05617184017846302,"score_gpt":0.34378712400197137,"score_spread":0.2876152838235083,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3174971506","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93060756,0.00006340408,0.06726513,0.000053817883,0.000011120988,0.000022501292,0.000057617865,0.00011711771,0.0018018149],"genre_scores_gemma":[0.9974068,0.000021425849,0.0023108856,0.000002419362,0.0000018176902,0.0000063821444,0.000010770963,0.0000032727255,0.00023625763],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999037,0.000026874437,0.0000075097246,0.00001711746,0.000027972857,0.000016743497],"domain_scores_gemma":[0.99975306,0.00009233689,0.0000666477,0.000030051593,0.000033979308,0.000024000154],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020782622,0.00033873133,0.0002700504,0.00045145673,0.00025860808,0.00042154055,0.00041543477,0.0006719204,0.00063499546],"category_scores_gemma":[0.0007007893,0.00017533032,0.0002633159,0.00029197626,0.00059135654,0.00036344162,0.000361931,0.00021287112,0.000070621485],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019422152,0.000032146247,0.00301092,0.000008905713,0.000006349427,0.000086321044,0.000027718404,0.98953617,0.0046609947,0.0006268137,0.000025306343,0.0019589385],"study_design_scores_gemma":[0.0000013589614,0.000008987915,0.00046528789,6.7751193e-7,0.0000011133243,0.000008541963,0.0000053478307,0.9991185,0.00028980896,0.000078193094,0.000020709014,0.0000014736172],"about_ca_topic_score_codex":0.0052849576,"about_ca_topic_score_gemma":0.0025228723,"teacher_disagreement_score":0.0052849576,"about_ca_system_score_codex":0.0003251496,"about_ca_system_score_gemma":0.00028294063,"threshold_uncertainty_score":0.010508418},"labels":[],"label_agreement":null},{"id":"W3175713072","doi":"10.1029/2021jb022035","title":"An Extended Rheological Map of Pāhoehoe—‘A‘ā Transition","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Ministero dell’Istruzione, dell’Università e della Ricerca","keywords":"Rheology; Shear rate; Crystallization; Thermodynamics; Shear (geology); Materials science; Viscosity; Dilatant; Mechanics; Mineralogy; Geology; Composite material; Physics","score_opus":0.03832650934724975,"score_gpt":0.3171706340821078,"score_spread":0.2788441247348581,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3175713072","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99773586,0.00007388495,0.0008949775,0.000018942103,0.0000024339809,0.0000084650355,0.00018969843,0.00004867317,0.0010270983],"genre_scores_gemma":[0.999337,0.0000214771,0.00037159905,0.0000066031125,0.0000018952109,0.0000053076783,0.00008954666,0.000008258859,0.00015825179],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99993217,0.000004589797,0.0000032979428,0.000026895073,0.00001260786,0.000020352683],"domain_scores_gemma":[0.9998,0.000036133697,0.000042102674,0.000025417707,0.00005648088,0.000039866194],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001076841,0.00012997095,0.00015424979,0.00048849836,0.00039162007,0.00044239892,0.00021652073,0.00030929464,0.0012845478],"category_scores_gemma":[0.000304171,0.00014071929,0.00014038397,0.0002659228,0.0004184094,0.00035646546,0.0002445173,0.00039092405,0.00013812297],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001785271,0.000036424997,0.01687901,0.00003985716,0.00001910654,0.00018265603,0.00035247076,0.0011396244,0.97659904,0.00044564425,0.00013049494,0.0039971494],"study_design_scores_gemma":[0.000030414752,0.0002600823,0.67715967,0.000025272637,0.00003284657,0.00039708382,0.0005762559,0.019432254,0.29609063,0.0008398884,0.0050963284,0.00005921642],"about_ca_topic_score_codex":0.0022531,"about_ca_topic_score_gemma":0.0015298941,"teacher_disagreement_score":0.0022531,"about_ca_system_score_codex":0.0002718937,"about_ca_system_score_gemma":0.00014475234,"threshold_uncertainty_score":0.0044800043},"labels":[],"label_agreement":null},{"id":"W3176492303","doi":"","title":"Imaging major Canadian sedimentary basins and their adjacent structures using ambient seismic noise (and other applications of seismic noise)","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismic noise; Geology; Noise (video); Seismology; Sedimentary basin; Ambient noise level; Acoustics; Geomorphology; Sound (geography); Computer science; Physics","score_opus":0.023578944198624455,"score_gpt":0.2891108622946873,"score_spread":0.26553191809606286,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3176492303","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97176695,0.00029830902,0.012500249,0.0002963378,0.00003580539,0.000030267558,0.0019190817,0.00027151994,0.012881543],"genre_scores_gemma":[0.9815763,0.0002741235,0.013104511,0.000047516285,0.000015096431,0.000007929431,0.0007320005,0.000040771174,0.0042016516],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99982125,0.000007585733,0.0000034329132,0.00002871373,0.000078509416,0.0000605225],"domain_scores_gemma":[0.99978465,0.000013804757,0.000013218737,0.000007210052,0.00015778665,0.000023273711],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019375095,0.00032104514,0.0001853777,0.0012539708,0.0009989956,0.0007365321,0.00033633853,0.0002972627,0.0010690261],"category_scores_gemma":[0.0005578168,0.00017132518,0.00016078404,0.0015948685,0.00028476462,0.00031484652,0.0004955088,0.00024150964,0.00017330305],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000919213,0.00021441405,0.35524705,0.00025640868,0.00024423603,0.00081535947,0.0015508421,0.06992815,0.22155154,0.004405237,0.010851788,0.33401567],"study_design_scores_gemma":[0.00006168376,0.000088898756,0.82871467,0.000037070746,0.00016559509,0.00035254963,0.0014649081,0.12867716,0.024298808,0.0010935584,0.014945127,0.00010001373],"about_ca_topic_score_codex":0.87836015,"about_ca_topic_score_gemma":0.96724975,"teacher_disagreement_score":0.12163985,"about_ca_system_score_codex":0.0018566118,"about_ca_system_score_gemma":0.0061833393,"threshold_uncertainty_score":0.24471235},"labels":[],"label_agreement":null},{"id":"W3187398051","doi":"10.1029/2021jb022445","title":"Modification of Lithospheric Mantle by Melts/Fluids With Different Sulfur Fugacities During the Wilson Cycle: Insights From Lesvos and Global Ophiolitic Peridotites","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"National Key Research and Development Program of China; Higher Education Discipline Innovation Project; National Natural Science Foundation of China","keywords":"Geology; Mantle (geology); Geochemistry; Lithosphere; Peridotite; Subduction; Mantle wedge; Partial melting; Radiogenic nuclide; Mid-ocean ridge; Rift; Ophiolite; Basalt; Trace element; Tectonics; Paleontology","score_opus":0.017478853556356217,"score_gpt":0.253615340752306,"score_spread":0.2361364871959498,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3187398051","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995122,0.000070632894,0.000022820688,0.0000051691527,4.096949e-7,0.0000015482648,0.00008813944,0.0000040391924,0.0002951005],"genre_scores_gemma":[0.99964,0.00004808282,0.000041413274,0.0000036454962,0.0000011042939,0.0000015965227,0.00012952878,0.000003262545,0.00013147914],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999459,0.0000042331253,0.00000473872,0.000019150038,0.000010577835,0.000015302816],"domain_scores_gemma":[0.99990773,0.000008945278,0.000039988692,0.000005986922,0.000018131188,0.000019248695],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001057656,0.00021852629,0.0002149982,0.0015660297,0.00027470442,0.00059685647,0.00015181428,0.00022201233,0.0008639922],"category_scores_gemma":[0.00018931986,0.00015094734,0.00020663161,0.000643659,0.00041112964,0.0002648692,0.00049405167,0.000103121005,0.00012006445],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002639825,0.000021327158,0.8261958,0.00005362557,0.00008911683,0.00029988587,0.0009367278,0.00030522878,0.16556886,0.000106108695,0.000046961133,0.0061123297],"study_design_scores_gemma":[0.0000024691358,0.000020733112,0.9976803,0.0000022047993,0.000009275411,0.00006336526,0.00032263083,0.00018804664,0.0014713439,0.000022049877,0.00021566173,0.0000019373167],"about_ca_topic_score_codex":0.0076624723,"about_ca_topic_score_gemma":0.01056645,"teacher_disagreement_score":0.0076624723,"about_ca_system_score_codex":0.0003949561,"about_ca_system_score_gemma":0.00017503515,"threshold_uncertainty_score":0.015235722},"labels":[],"label_agreement":null},{"id":"W3192902513","doi":"10.1029/2021jb021960","title":"Surface‐Wave Tomography of the Northern Canadian Cordillera Using Earthquake Rayleigh Wave Group Velocities","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; University of Ottawa; McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Seismology; Lithosphere; Crust; Asthenosphere; Craton; Low-velocity zone; Mantle (geology); Rayleigh wave; Seismic tomography; Group velocity; Geophysics; Surface wave; Tectonics","score_opus":0.05143600704837931,"score_gpt":0.27745415936504186,"score_spread":0.22601815231666256,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3192902513","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9853021,0.0002481721,0.0029371812,0.0001992182,0.000013905688,0.000032832417,0.0029169417,0.00036290206,0.007986813],"genre_scores_gemma":[0.99531555,0.00008774434,0.0025332093,0.000015951036,0.0000050125955,0.000009501582,0.0010820173,0.000021475993,0.00092965027],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989974,0.0000044980525,0.0000026447228,0.00002394857,0.000042605658,0.000026655583],"domain_scores_gemma":[0.9997861,0.00001418727,0.000031607586,0.0000128221545,0.0001259885,0.000029350598],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000119847566,0.0005125517,0.00015907624,0.0018582543,0.0007874112,0.00085124513,0.0005994584,0.00025896312,0.0018055642],"category_scores_gemma":[0.0006233942,0.00021356843,0.00024442756,0.001988852,0.0002696087,0.00020948243,0.00047578514,0.00026106607,0.00028075703],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033800703,0.00012113961,0.69340897,0.00012190008,0.0002602135,0.00054523273,0.0012400757,0.09205745,0.052296765,0.0023484435,0.0046420223,0.15261987],"study_design_scores_gemma":[0.000027623932,0.000015268077,0.88242793,0.000021827522,0.00003498325,0.00004686838,0.0004032087,0.111236334,0.0021369075,0.0003019208,0.0033094562,0.00003760141],"about_ca_topic_score_codex":0.9485866,"about_ca_topic_score_gemma":0.9619416,"teacher_disagreement_score":0.051413417,"about_ca_system_score_codex":0.00437692,"about_ca_system_score_gemma":0.005193286,"threshold_uncertainty_score":0.10343236},"labels":[],"label_agreement":null},{"id":"W3193150665","doi":"10.1029/2020jb020562","title":"Three‐Dimensional Inversion of Magnetotelluric Data for a Resistivity Model With Arbitrary Anisotropy","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"China Scholarship Council; National Natural Science Foundation of China","keywords":"Anisotropy; Magnetotellurics; Isotropy; Inversion (geology); Electrical resistivity and conductivity; Geology; Geophysics; Synthetic data; Algorithm; Physics; Computer science; Optics; Seismology","score_opus":0.09440622602076437,"score_gpt":0.34446846625705513,"score_spread":0.25006224023629076,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3193150665","genre_codex":"empirical","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7229101,0.000074443495,0.2735051,0.00021828907,0.000027046011,0.000029554472,0.00032521968,0.0008177161,0.0020924457],"genre_scores_gemma":[0.95588654,0.000026345377,0.04356932,0.000017538829,0.0000054779575,0.000013035689,0.00021234302,0.000032192584,0.00023730203],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998994,0.00003028797,0.0000072935204,0.000019055004,0.000032017542,0.000011982728],"domain_scores_gemma":[0.9997036,0.00011845568,0.000036270103,0.000049564005,0.00007382142,0.000018418714],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004440854,0.000418275,0.00023726354,0.0003566922,0.0002146328,0.00048719975,0.00035673284,0.0003826071,0.00034886788],"category_scores_gemma":[0.0011932139,0.00019854147,0.0004575634,0.00052297127,0.00029635153,0.0003835083,0.00027567256,0.00042368923,0.00010467636],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008680761,0.00005004376,0.0058601825,0.000040609153,0.000042478554,0.00015927931,0.00009224306,0.9377303,0.03400176,0.0018115602,0.0004120372,0.019712664],"study_design_scores_gemma":[0.000006722974,0.000006858293,0.0008763521,0.0000015573999,0.0000029883843,0.000015605363,0.000010740956,0.99584866,0.0028139337,0.00021335584,0.00019652864,0.000006738476],"about_ca_topic_score_codex":0.008091533,"about_ca_topic_score_gemma":0.0063731656,"teacher_disagreement_score":0.008091533,"about_ca_system_score_codex":0.00037614725,"about_ca_system_score_gemma":0.00061277155,"threshold_uncertainty_score":0.016088903},"labels":[],"label_agreement":null},{"id":"W3193317780","doi":"10.1029/2021jb022245","title":"The Change in Geomechanical Properties of Gas Saturated Methane Hydrate‐Bearing Sand Resulting From Water Saturation","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Stantec (Canada); University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Hydrate; Saturation (graph theory); Clathrate hydrate; Methane; Chemistry; Pore water pressure; Mineralogy; Geotechnical engineering; Geology; Materials science","score_opus":0.061934053785011364,"score_gpt":0.313273148100673,"score_spread":0.25133909431566165,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3193317780","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992435,0.000024593177,0.00030236153,0.000005780064,0.0000016736743,0.0000054100083,0.00009741439,0.0000123276395,0.00030691072],"genre_scores_gemma":[0.9992785,0.000020214555,0.00024389048,0.000005180236,5.851261e-7,0.0000055231844,0.00009326262,0.0000041019975,0.0003487453],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99990666,0.000007814623,0.000007757167,0.000011688747,0.00004532535,0.000020749814],"domain_scores_gemma":[0.9997639,0.000058700818,0.000058133788,0.000014521629,0.000057679194,0.00004703115],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001697759,0.00024507957,0.00014931924,0.0002782163,0.00018715604,0.00019382226,0.00017210258,0.00017433027,0.0015009564],"category_scores_gemma":[0.00030946865,0.00021299212,0.00012895362,0.0002054084,0.00043146018,0.00015443051,0.00015534634,0.00023375308,0.00012634452],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000119798744,0.000008571414,0.0027181199,0.00002067931,0.0000055764394,0.000081195045,0.0000545332,0.00038139283,0.99580234,0.000025712166,0.000013531191,0.00076854177],"study_design_scores_gemma":[0.0000058369883,0.00024306813,0.06030397,0.000004315046,0.000011504113,0.000087427616,0.00024150318,0.0021440084,0.9365548,0.000024341065,0.0003697665,0.000009562783],"about_ca_topic_score_codex":0.0034449154,"about_ca_topic_score_gemma":0.0067315856,"teacher_disagreement_score":0.0034449154,"about_ca_system_score_codex":0.00027516627,"about_ca_system_score_gemma":0.00018762113,"threshold_uncertainty_score":0.006849706},"labels":[],"label_agreement":null},{"id":"W3194491437","doi":"10.1029/2021jb022839","title":"Raton Basin Induced Seismicity Is Hosted by Networks of Short Basement Faults and Mimics Tectonic Earthquake Statistics","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Science Foundation","keywords":"Induced seismicity; Seismology; Geology; Tectonics; Structural basin; Fault (geology); Slip (aerodynamics); Basement; Geomorphology","score_opus":0.03966873536569286,"score_gpt":0.3138336121222472,"score_spread":0.2741648767565543,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3194491437","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9935382,0.00007666857,0.0002542601,0.000053629567,0.000009044148,0.000008140071,0.001981849,0.000076427736,0.0040018456],"genre_scores_gemma":[0.99647105,0.000038922233,0.00024919555,0.000011792754,0.0000067016454,0.0000056678487,0.0021555775,0.000015694717,0.0010454882],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988127,0.000010915405,0.000008485859,0.000037983504,0.00002479739,0.000036582307],"domain_scores_gemma":[0.9996495,0.000033462158,0.00014203369,0.000031575943,0.00009940025,0.00004396245],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013517786,0.0002279359,0.00013099806,0.0013946964,0.00021149238,0.0005087051,0.00021562044,0.00011846446,0.003913747],"category_scores_gemma":[0.00050527207,0.000086712564,0.00016298238,0.001096023,0.0002197626,0.00023333888,0.00040136007,0.00011261091,0.000384853],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012427398,0.000030614956,0.96701753,0.000067352295,0.00006148641,0.00027109965,0.0003445944,0.002508354,0.005070475,0.00042098138,0.003242315,0.02084108],"study_design_scores_gemma":[0.0000031369077,0.000014434909,0.99302226,0.00001441756,0.000012125655,0.00007719641,0.0002624559,0.004062981,0.0003767157,0.00006770769,0.0020803353,0.0000062777026],"about_ca_topic_score_codex":0.07408861,"about_ca_topic_score_gemma":0.20135532,"teacher_disagreement_score":0.07408861,"about_ca_system_score_codex":0.0005859321,"about_ca_system_score_gemma":0.00048823393,"threshold_uncertainty_score":0.14731473},"labels":[],"label_agreement":null},{"id":"W3195487486","doi":"10.1029/2020jb021573","title":"Toward Waveform‐Based Characterization of Slab &amp; Mantle Wedge (SAM) Earthquakes","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Seismology; Subduction; Seismogram; Classification of discontinuities; Slab; Mantle (geology); Discontinuity (linguistics); Mantle wedge; Seismic array; Crust; Geophysics; Tectonics","score_opus":0.08176908914775273,"score_gpt":0.3249869136564549,"score_spread":0.24321782450870216,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3195487486","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.86642385,0.00022276177,0.12473141,0.000095716765,0.000023999904,0.000103018094,0.004569546,0.0016914441,0.0021382978],"genre_scores_gemma":[0.8991849,0.00013095881,0.09524686,0.000018243774,0.000025840862,0.00003940028,0.0046952097,0.00012786941,0.00053078233],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9998344,0.000033272372,0.000022722008,0.000053929554,0.000031327556,0.00002425666],"domain_scores_gemma":[0.99895334,0.00023805922,0.0001983373,0.00015573956,0.0003539886,0.00010043062],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005894818,0.00047991026,0.00027052325,0.0045614084,0.00010921741,0.0006907587,0.0003854936,0.00044838866,0.0010068595],"category_scores_gemma":[0.0016397724,0.00016164534,0.00035046766,0.0016681921,0.0001242942,0.0003954947,0.0006030023,0.0002927601,0.00085266907],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044102868,0.00033682174,0.29777125,0.0002578609,0.00012174864,0.00036632543,0.00040266526,0.024079373,0.32793516,0.00085468416,0.001575951,0.3458571],"study_design_scores_gemma":[0.000057299367,0.00020777932,0.57025445,0.000043610893,0.00007285739,0.0003752937,0.00044040487,0.37516847,0.04873951,0.0009108828,0.0036794308,0.000050121784],"about_ca_topic_score_codex":0.0030154036,"about_ca_topic_score_gemma":0.0039807423,"teacher_disagreement_score":0.0045614084,"about_ca_system_score_codex":0.00016491002,"about_ca_system_score_gemma":0.0002979843,"threshold_uncertainty_score":0.005995691},"labels":[],"label_agreement":null},{"id":"W3198700235","doi":"10.1029/2021jb022292","title":"New Paleointensities From the Skinner Cove Formation, Newfoundland, Suggest a Changing State of the Geomagnetic Field at the Ediacaran‐Cambrian Transition","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"Natural Environment Research Council; Sight Research UK; Leverhulme Trust","keywords":"Geology; Earth's magnetic field; Paleontology; Conglomerate; Paleomagnetism; Geomagnetic pole; Cove; Geophysics; Magnetostratigraphy; Field (mathematics); Geomorphology; Magnetic field; Sedimentary rock","score_opus":0.013757791749600533,"score_gpt":0.2698342114275686,"score_spread":0.25607641967796807,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3198700235","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99701655,0.00018026141,0.00014614758,0.000026402588,0.0000024736166,0.0000047472586,0.00031842059,0.000009554462,0.0022954242],"genre_scores_gemma":[0.9988662,0.000056316516,0.000169602,0.0000114352415,0.0000015271044,0.0000027632727,0.0002293796,0.0000030863657,0.0006597201],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987733,0.000005639071,0.0000058077185,0.000045262514,0.000024053,0.000041794443],"domain_scores_gemma":[0.9997316,0.000030803807,0.00006308222,0.000020724963,0.00010890964,0.000044915374],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023166124,0.0002051111,0.00017659133,0.00187711,0.0009790554,0.0008067229,0.00034481194,0.00015012072,0.0021499773],"category_scores_gemma":[0.00035944337,0.0002084734,0.00012515574,0.0012178133,0.0010046919,0.00025292742,0.00048972195,0.00027190847,0.00017415681],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002551849,0.000034338533,0.89654744,0.00007610553,0.000112294896,0.00059942063,0.003926868,0.00042490862,0.0717368,0.00040086766,0.0005161719,0.025369491],"study_design_scores_gemma":[0.000001373953,0.0000055942533,0.9988481,0.000004327866,0.0000040277755,0.000050973456,0.0002433624,0.000042912125,0.00041632677,0.0000057405437,0.0003754096,0.000001834774],"about_ca_topic_score_codex":0.66647714,"about_ca_topic_score_gemma":0.9098984,"teacher_disagreement_score":0.33352286,"about_ca_system_score_codex":0.0031949938,"about_ca_system_score_gemma":0.0008082846,"threshold_uncertainty_score":0.6709741},"labels":[],"label_agreement":null},{"id":"W3201228016","doi":"10.1029/2021jb022177","title":"Seismic Velocity Structure Along and Across the Ultraslow‐Spreading Southwest Indian Ridge at 64°30′E Showcases Flipping Detachment Faults","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Institut national des sciences de l'Univers; Natural Sciences and Engineering Research Council of Canada; Agence Nationale de la Recherche","keywords":"Geology; Seafloor spreading; Lithosphere; Detachment fault; Ridge; Mid-Atlantic Ridge; Seismology; Ridge push; Mid-ocean ridge; Seismometer; Volcano; Mantle (geology); Crust; Perpendicular; Geophysics; Tectonics; Hydrothermal circulation; Geometry; Paleontology; Extensional definition","score_opus":0.03497886114568297,"score_gpt":0.321850281704336,"score_spread":0.286871420558653,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3201228016","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984068,0.000014401089,0.0005253848,0.000023963448,0.000002706375,0.0000035932133,0.00022006997,0.000058546997,0.0007445425],"genre_scores_gemma":[0.9990879,0.00001079482,0.0003379648,0.0000031316483,0.0000011605977,0.000002616877,0.00033960995,0.0000043286577,0.00021248743],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999529,0.000004157824,0.000002568462,0.000013847444,0.000010860674,0.000015585918],"domain_scores_gemma":[0.9999161,0.00000871957,0.000020945909,0.000013735404,0.000016807362,0.000023726312],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000046566853,0.00025345996,0.00014009433,0.00042542,0.00023750616,0.0005283386,0.00037479884,0.0003017296,0.001187293],"category_scores_gemma":[0.00018401112,0.00020559788,0.00033362082,0.00037832343,0.00020832835,0.0001587058,0.00031236795,0.00022016447,0.00023104867],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036526358,0.00016415822,0.80540985,0.00004905991,0.00011532869,0.00065638934,0.0008931135,0.118609056,0.04109564,0.0007567239,0.00093845394,0.030946938],"study_design_scores_gemma":[0.000034544635,0.000072232135,0.84604645,0.000012536368,0.00003611257,0.00015469891,0.00054492516,0.14973886,0.0020657151,0.00031296804,0.0009484713,0.000032581676],"about_ca_topic_score_codex":0.052400235,"about_ca_topic_score_gemma":0.049978092,"teacher_disagreement_score":0.052400235,"about_ca_system_score_codex":0.00041497682,"about_ca_system_score_gemma":0.00045599285,"threshold_uncertainty_score":0.10419047},"labels":[],"label_agreement":null},{"id":"W3201463835","doi":"10.1029/2021jb022343","title":"Exploration of Data Space Through Trans‐Dimensional Sampling: A Case Study of 4D Seismics","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"St. John’s Health Sciences Centre; Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada; Istituto Nazionale di Geofisica e Vulcanologia; Austrian Science Fund","keywords":"Markov chain Monte Carlo; Sampling (signal processing); Computer science; Data mining; Context (archaeology); Bayesian probability; Synthetic data; Noise (video); Algorithm; Posterior probability; Covariance matrix; Monte Carlo method; Covariance; Geology; Statistics; Mathematics; Artificial intelligence; Filter (signal processing); Computer vision","score_opus":0.26745728674883124,"score_gpt":0.41761394674668156,"score_spread":0.15015665999785033,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3201463835","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.26172185,0.00047874582,0.73337764,0.0008351307,0.000028823468,0.00015158302,0.000455298,0.00034159663,0.0026092646],"genre_scores_gemma":[0.52725285,0.00031367972,0.4710463,0.000081723185,0.000026155747,0.0001141984,0.0004083655,0.00008627401,0.00067043345],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9965894,0.0018758264,0.0001991625,0.00035418826,0.0008295099,0.00015199013],"domain_scores_gemma":[0.9875728,0.008703035,0.0007151391,0.0016199757,0.0010701567,0.000318827],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0042029424,0.0005208885,0.00061101874,0.001381443,0.00066996476,0.0015225498,0.0012868623,0.0013881538,0.0008270851],"category_scores_gemma":[0.012902296,0.0004148469,0.000818162,0.0026147484,0.0020638884,0.0015402267,0.0022396466,0.0011342214,0.0001610567],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000560706,0.000371313,0.07202639,0.00056623796,0.00020991894,0.004497597,0.0049490556,0.62160975,0.015842918,0.060341485,0.0021049448,0.2169197],"study_design_scores_gemma":[0.000049627226,0.00024702784,0.010585875,0.00009070502,0.000051264276,0.001905382,0.0016506165,0.9290335,0.011923332,0.030150814,0.01422101,0.00009085202],"about_ca_topic_score_codex":0.007211717,"about_ca_topic_score_gemma":0.009186812,"teacher_disagreement_score":0.007211717,"about_ca_system_score_codex":0.00066181825,"about_ca_system_score_gemma":0.00090733095,"threshold_uncertainty_score":0.022227585},"labels":[],"label_agreement":null},{"id":"W3201485237","doi":"10.1029/2021jb021950","title":"Seismoelectric and Electroseismic Modeling in Stratified Porous Media With a Shallow or Ground Surface Source","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"National Natural Science Foundation of China","keywords":"Inversion (geology); Electrokinetic phenomena; Wavelength; Geology; Computer science; Trough (economics); Algorithm; Geophysics; Optics; Physics; Seismology; Materials science; Tectonics","score_opus":0.06066656730118207,"score_gpt":0.3172228831479756,"score_spread":0.2565563158467935,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3201485237","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.58441395,0.00018655996,0.41169602,0.00009775188,0.000027921014,0.00003415546,0.00011784044,0.0002556939,0.0031700754],"genre_scores_gemma":[0.9832327,0.000088762106,0.015562704,0.000013544037,0.000007086825,0.000021694455,0.000041226675,0.000011783491,0.0010206552],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999275,0.000016286045,0.0000050895787,0.000013069942,0.000021091393,0.000016915117],"domain_scores_gemma":[0.99983823,0.00006303855,0.00003604387,0.000016499978,0.000031138414,0.000015078678],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016918861,0.00041796832,0.00022982356,0.00026703867,0.00016799536,0.00040746276,0.00052201207,0.00049411977,0.00037451988],"category_scores_gemma":[0.0005710092,0.00017393642,0.00036024008,0.00026928034,0.00042692272,0.00056173006,0.00044558506,0.00029079642,0.00007182595],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003583109,0.000031199364,0.0021853908,0.000020707526,0.000017541897,0.00015924117,0.000033264998,0.96957517,0.019824449,0.0035623051,0.000059384914,0.004495529],"study_design_scores_gemma":[0.0000023225327,0.0000072823304,0.00026638815,8.5987904e-7,0.0000022065046,0.000007999472,0.00000691332,0.9981768,0.0011371435,0.00033913512,0.00005042421,0.0000025742415],"about_ca_topic_score_codex":0.0076432447,"about_ca_topic_score_gemma":0.0035679026,"teacher_disagreement_score":0.0076432447,"about_ca_system_score_codex":0.00040268194,"about_ca_system_score_gemma":0.0005184139,"threshold_uncertainty_score":0.0151975155},"labels":[],"label_agreement":null},{"id":"W3202395399","doi":"10.1029/2021jb022539","title":"What Controls the Presence and Characteristics of Aftershocks in Rock Fracture in the Lab?","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Hotchkiss Brain Institute; University of Calgary","funders":"AXA Research Fund; Deutsche Forschungsgemeinschaft; Alexander von Humboldt-Stiftung","keywords":"Aftershock; Geology; Seismology; Induced seismicity; Differential stress; Acoustic emission; Slip (aerodynamics); Microseism; Fracture (geology); Deformation (meteorology); Geotechnical engineering; Physics","score_opus":0.030305041288087455,"score_gpt":0.3089532536213502,"score_spread":0.2786482123332627,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3202395399","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987527,0.00007213791,0.00065278943,0.00001523281,0.0000023692955,0.0000052587284,0.000074229334,0.000017627919,0.00040767156],"genre_scores_gemma":[0.9996903,0.000027840617,0.00011444344,0.000009241394,0.0000023510413,0.0000046880787,0.000050708135,0.0000042188544,0.00009611368],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9997811,0.00003551012,0.00001257133,0.00006455698,0.000035162415,0.00007116515],"domain_scores_gemma":[0.9991905,0.00019954678,0.0003085305,0.000077398705,0.00008156499,0.00014241476],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034142568,0.00015128206,0.0003266101,0.00028554542,0.00010604179,0.00055827317,0.00024416507,0.00026680887,0.0015911653],"category_scores_gemma":[0.0010422529,0.00014499312,0.00015580888,0.00019209247,0.00031310917,0.00031952118,0.00033476556,0.00020152864,0.00022762318],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000921591,0.00018254523,0.22024132,0.000104424995,0.00007859069,0.00026003108,0.00014954938,0.001764253,0.76259506,0.00030870576,0.00014027122,0.013253524],"study_design_scores_gemma":[0.000012027917,0.0005421337,0.945693,0.000010005681,0.000039594604,0.00014235903,0.00033592887,0.005557422,0.046975046,0.0002592663,0.00041398645,0.000019182286],"about_ca_topic_score_codex":0.0006625336,"about_ca_topic_score_gemma":0.0006737351,"teacher_disagreement_score":0.0015911653,"about_ca_system_score_codex":0.00022931684,"about_ca_system_score_gemma":0.00012370407,"threshold_uncertainty_score":0.005322993},"labels":[],"label_agreement":null},{"id":"W3203067527","doi":"10.1029/2021jb022523","title":"Cataloging Tectonic Tremor Energy Radiation in the Cascadia Subduction Zone","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Subduction; Geology; Seismology; Episodic tremor and slip; Tectonics; Epicenter; Terrane; Slip (aerodynamics)","score_opus":0.04064541655784556,"score_gpt":0.3099892620855354,"score_spread":0.26934384552768986,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3203067527","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99420565,0.0001951009,0.0005613408,0.000031887823,0.000003814695,0.000017208786,0.0025698892,0.00013268637,0.0022824872],"genre_scores_gemma":[0.993509,0.00019241219,0.00082697824,0.000007127733,0.0000057037473,0.000017594148,0.0047380845,0.000016986494,0.0006861084],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998056,0.000013953091,0.00002678798,0.000060195922,0.00006927947,0.000024166742],"domain_scores_gemma":[0.9992461,0.000068376154,0.00023819963,0.000078161705,0.00022074893,0.0001483639],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027200105,0.0004112982,0.00018666078,0.004703421,0.00036507123,0.00052476715,0.00026415547,0.00016106898,0.0011685877],"category_scores_gemma":[0.0008680116,0.0001687298,0.00025352376,0.0038743585,0.00021739182,0.00022617888,0.00072917115,0.00014578261,0.00027025875],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000042090527,0.000012161186,0.9795363,0.00005210599,0.00006138877,0.00016294872,0.00051023107,0.0013932341,0.0035686083,0.00006207658,0.00057762384,0.0140211275],"study_design_scores_gemma":[0.0000017355009,0.000007504857,0.9984097,0.000006328879,0.000009760372,0.000031226133,0.00010719913,0.0005214187,0.00019537863,0.000023069611,0.0006837977,0.0000029307882],"about_ca_topic_score_codex":0.054782927,"about_ca_topic_score_gemma":0.08316802,"teacher_disagreement_score":0.054782927,"about_ca_system_score_codex":0.00070871675,"about_ca_system_score_gemma":0.0005247836,"threshold_uncertainty_score":0.108928084},"labels":[],"label_agreement":null},{"id":"W3210751055","doi":"10.1029/2021jb022569","title":"The Spatial Relationship Between Contemporaneous Tremor Detections in Relatively Low‐ and High‐Frequency Bands","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Offset (computer science); Low frequency; Geology; Subduction; Guard (computer science); Physics; Seismology; Energy (signal processing); Geodesy; Acoustics; Computer science; Telecommunications","score_opus":0.06610620334319858,"score_gpt":0.3241029477832629,"score_spread":0.25799674444006426,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3210751055","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985538,0.00010986856,0.0004977908,0.000010928663,0.0000043020614,0.0000023494617,0.00015766727,0.000014777403,0.000648564],"genre_scores_gemma":[0.9993099,0.00002681525,0.00027731032,0.0000034762475,0.000003378526,0.0000017207196,0.00016776484,0.0000033603226,0.00020628463],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999778,0.000017554003,0.000017996144,0.00008625579,0.000057412624,0.000042760515],"domain_scores_gemma":[0.99800855,0.0006397266,0.00057277444,0.0001410341,0.00049169693,0.00014631839],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027549756,0.00010985499,0.00016089508,0.0011371126,0.00027776946,0.00054191967,0.00023811315,0.00025709614,0.0016447697],"category_scores_gemma":[0.0025232502,0.00014416581,0.000100246034,0.0008623592,0.000230183,0.00021399852,0.0003629724,0.0002383021,0.0002858159],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010618164,0.00001932992,0.96971107,0.000031173877,0.00006508419,0.00010309099,0.0003378949,0.0004297585,0.016212653,0.00007917577,0.00012699542,0.012777499],"study_design_scores_gemma":[0.0000013897226,0.000009266236,0.99878865,0.0000038765215,0.000008465374,0.00003944147,0.00009120137,0.00036328047,0.0005406466,0.00001138642,0.0001403931,0.0000019909153],"about_ca_topic_score_codex":0.022350866,"about_ca_topic_score_gemma":0.053056963,"teacher_disagreement_score":0.022350866,"about_ca_system_score_codex":0.00025174685,"about_ca_system_score_gemma":0.00018021453,"threshold_uncertainty_score":0.04444158},"labels":[],"label_agreement":null},{"id":"W3213276065","doi":"10.1029/2021jb022201","title":"New Insights Into the Rift to Drift Transition Across the Northeastern Nova Scotian Margin From Wide‐Angle Seismic Waveform Inversion and Reflection Imaging","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Division of Ocean Sciences; Ocean Frontier Institute","keywords":"Geology; Continental margin; Oceanic crust; Seismology; Rift; Magmatism; Continental crust; Mantle (geology); Breakup; Crust; Basement; Inversion (geology); Paleontology; Subduction; Tectonics","score_opus":0.03017986193174319,"score_gpt":0.30963600026370663,"score_spread":0.2794561383319634,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3213276065","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996725,0.000079781945,0.00067827554,0.000041999694,0.00000419314,0.000008796313,0.00037675723,0.000029687812,0.002055602],"genre_scores_gemma":[0.99906343,0.00003478791,0.00033398956,0.000005566744,0.0000015258946,0.0000014627732,0.00020971891,0.0000062583817,0.0003431962],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999604,0.0000035431824,0.0000020574496,0.000011840121,0.000009062254,0.000013055983],"domain_scores_gemma":[0.99988365,0.000018737474,0.000024804023,0.000009043515,0.000039827537,0.000023990291],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010165978,0.00019415833,0.00008872495,0.00065176684,0.00021372385,0.0005282029,0.00014568855,0.00013781447,0.001398109],"category_scores_gemma":[0.00040549357,0.00015294572,0.00016806778,0.00049303105,0.00021116696,0.000142443,0.0002650253,0.00012167792,0.00017140737],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000187671,0.00005587589,0.8475033,0.00007278019,0.00008763969,0.0011191731,0.0010025905,0.020082576,0.0845278,0.0006534432,0.0008524925,0.043854654],"study_design_scores_gemma":[0.000007962968,0.000007677963,0.9817359,0.000010119642,0.000009386312,0.00006628391,0.00028295146,0.016730143,0.00061326835,0.00006614316,0.0004642761,0.0000059636745],"about_ca_topic_score_codex":0.36586136,"about_ca_topic_score_gemma":0.5243254,"teacher_disagreement_score":0.63413864,"about_ca_system_score_codex":0.00081667275,"about_ca_system_score_gemma":0.00092935166,"threshold_uncertainty_score":0.7274636},"labels":[],"label_agreement":null},{"id":"W3215033000","doi":"10.1029/2021jb022161","title":"Continuous Tremor Activity With Stable Polarization Direction Following the 2014 Large Slow Slip Event in the Hikurangi Subduction Margin Offshore New Zealand","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Golder Associates (Canada)","funders":"Japan Society for the Promotion of Science; University of Tokyo; Ministry of Education, Culture, Sports, Science and Technology; National Science Foundation","keywords":"Seismology; Geology; Episodic tremor and slip; Subduction; Slip (aerodynamics); Seismometer; Submarine pipeline; Seamount; Plate tectonics; Tectonics; Paleontology; Oceanography","score_opus":0.022386872690543576,"score_gpt":0.290037639695184,"score_spread":0.2676507670046404,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3215033000","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994646,0.000014135123,0.000039247127,0.000008915336,0.0000016265493,0.0000050313456,0.00013170879,0.000002812227,0.00033188885],"genre_scores_gemma":[0.9994497,0.000028586765,0.00006461848,0.000004597419,0.0000027696399,0.000005850854,0.00019113004,0.0000011994068,0.0002514761],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998957,0.000006948551,0.000007678314,0.000024601226,0.000040115174,0.000024965439],"domain_scores_gemma":[0.99960035,0.000032301214,0.00015549838,0.000020539932,0.00011243588,0.000078780715],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017747909,0.00018956137,0.00022468294,0.00085903076,0.0003804733,0.0003845475,0.00020622005,0.00023178851,0.0007939341],"category_scores_gemma":[0.00065364985,0.00014681017,0.00013404217,0.00077622157,0.0005112523,0.00020509213,0.0005618125,0.0002345675,0.00015641653],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039849256,0.0001038338,0.9386743,0.00005261353,0.000057930105,0.0012012037,0.0024032816,0.00036433208,0.04512136,0.000046527068,0.00042122847,0.011154975],"study_design_scores_gemma":[0.0000022283853,0.000024619903,0.9993549,0.0000019587771,0.0000030733624,0.00002934846,0.00024021562,0.00010010344,0.00016701203,0.0000034336722,0.00007118457,0.0000019462457],"about_ca_topic_score_codex":0.078392856,"about_ca_topic_score_gemma":0.13550511,"teacher_disagreement_score":0.078392856,"about_ca_system_score_codex":0.0005353283,"about_ca_system_score_gemma":0.000409513,"threshold_uncertainty_score":0.15587312},"labels":[],"label_agreement":null},{"id":"W3217208577","doi":"10.1029/2021jb023013","title":"3D Active Source Seismic Imaging of the Alpine Fault Zone and the Whataroa Glacial Valley in New Zealand","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta; University of Calgary","funders":"Canada Research Chairs; Technische Universität Bergakademie Freiberg; Victoria University of Wellington; Victoria University; Deutsche Forschungsgemeinschaft; University of Alberta; Natural Sciences and Engineering Research Council of Canada; Government of Alberta; Earthquake Commission; University of Otago","keywords":"Geology; Borehole; Seismology; Fault (geology); Geophysical imaging; Tectonics; Drilling; Glacial period; Trough (economics); Reflector (photography); Geomorphology; Paleontology","score_opus":0.020964325325717216,"score_gpt":0.2870343089268938,"score_spread":0.26606998360117656,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3217208577","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99075085,0.0002057326,0.0011026686,0.000112012436,0.000013244659,0.00006649822,0.0020068414,0.00010214033,0.0056400555],"genre_scores_gemma":[0.99420726,0.0002170492,0.0029206425,0.000029879935,0.000012869597,0.000034320987,0.00093228207,0.00003032004,0.0016152972],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999219,0.0000025205122,0.0000031452216,0.000018616713,0.000035340105,0.000018612382],"domain_scores_gemma":[0.9998847,0.000010980341,0.000029537397,0.0000068016525,0.000040500672,0.000027448013],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011653834,0.00039027762,0.0002469683,0.0021977099,0.00039443534,0.0009211172,0.00031413353,0.00037548834,0.0026310184],"category_scores_gemma":[0.00026874535,0.0003732672,0.00025050947,0.0015110774,0.00028382544,0.0002895551,0.00046882787,0.00028671246,0.00031966955],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006425725,0.00033177264,0.33148307,0.0005195138,0.00024611884,0.007073467,0.006617761,0.009907093,0.52475846,0.0006106849,0.0042606927,0.11354891],"study_design_scores_gemma":[0.000050716837,0.00005912341,0.98757625,0.000052180403,0.00004263725,0.00068257184,0.0014582892,0.0057571027,0.0018244059,0.000073793824,0.0023957784,0.000027087597],"about_ca_topic_score_codex":0.13575277,"about_ca_topic_score_gemma":0.29697597,"teacher_disagreement_score":0.13575277,"about_ca_system_score_codex":0.00055611215,"about_ca_system_score_gemma":0.0007090485,"threshold_uncertainty_score":0.26992518},"labels":[],"label_agreement":null},{"id":"W4200068194","doi":"10.1029/2021jb022729","title":"Initial Results From the Oman Drilling Project Multi‐Borehole Observatory: Petrogenesis and Ongoing Alteration of Mantle Peridotite in the Weathering Horizon","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Japan Agency for Marine-Earth Science and Technology; Natural Environment Research Council; Alfred P. Sloan Foundation; European Science Foundation; Sight Research UK; Japan Society for the Promotion of Science; NASA Astrobiology Institute; National Aeronautics and Space Administration; National Science Foundation","keywords":"Peridotite; Geology; Geochemistry; Mineral redox buffer; Weathering; Mantle (geology); Petrogenesis; Olivine; Silicate; Igneous rock; Mineralogy; Chemistry","score_opus":0.09202249813023554,"score_gpt":0.3280465536059384,"score_spread":0.23602405547570282,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200068194","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9938372,0.0002110792,0.00037747042,0.00011556692,0.000008195011,0.000032942822,0.0016662425,0.000019973133,0.0037313558],"genre_scores_gemma":[0.99629176,0.0001107573,0.0012259119,0.000046403762,0.00001749863,0.000019685463,0.0011071131,0.0000076024758,0.0011733223],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99973184,0.000051358715,0.00001299471,0.00004764995,0.000074267955,0.00008184402],"domain_scores_gemma":[0.99949515,0.00007599922,0.00013340224,0.00003683756,0.00017274173,0.000085731204],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006873181,0.00037524948,0.00011396155,0.0012226542,0.0006964586,0.00036011697,0.00020760993,0.0004032368,0.0007197284],"category_scores_gemma":[0.00054767734,0.00014115713,0.00013961464,0.0009388819,0.00024558994,0.00032511642,0.0004735985,0.0002032207,0.00012000847],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00058066286,0.00016433594,0.93844295,0.0000904212,0.000046622277,0.0006947084,0.0019541997,0.00081534375,0.02404497,0.00042424773,0.0013753121,0.031366274],"study_design_scores_gemma":[0.000004667187,0.000039723902,0.99553525,0.000007463309,0.000008689668,0.000040050774,0.00022982617,0.00025235998,0.0013452675,0.000025362366,0.0025079201,0.0000034582322],"about_ca_topic_score_codex":0.060742915,"about_ca_topic_score_gemma":0.17415304,"teacher_disagreement_score":0.060742915,"about_ca_system_score_codex":0.0013386892,"about_ca_system_score_gemma":0.00041761264,"threshold_uncertainty_score":0.12077868},"labels":[],"label_agreement":null},{"id":"W4205211984","doi":"10.1029/2021jb023002","title":"A Test of the Hypothesis That Syn‐Collisional Felsic Magmatism Contributes to Continental Crustal Growth Via Deep Learning Modeling and Principal Component Analysis of Big Geochemical Datasets","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Laurentian University","funders":"Chang'an University","keywords":"Magmatism; Continental crust; Felsic; Geology; Crust; Adakite; Igneous rock; Geochemistry; Earth science; Subduction; Continental arc; Continental collision; Oceanic crust; Mafic; Petrology; Paleontology; Tectonics","score_opus":0.03322134773230187,"score_gpt":0.26512081165879914,"score_spread":0.23189946392649727,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4205211984","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9692876,0.00015389721,0.028456079,0.0005011053,0.000026227912,0.000018573526,0.0004280067,0.00033185826,0.0007966646],"genre_scores_gemma":[0.99333054,0.000032608943,0.005570949,0.000049134513,0.000009748801,0.000009334336,0.0007124564,0.000014371003,0.0002708079],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99958533,0.00014206237,0.000018354236,0.00015809,0.000037293463,0.00005883188],"domain_scores_gemma":[0.99854654,0.0008927923,0.00013726413,0.0001439048,0.00016398435,0.00011547405],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0021886453,0.00065533747,0.00026404468,0.0005733925,0.00032727496,0.000860475,0.0006409575,0.00041433942,0.0008226814],"category_scores_gemma":[0.0030654708,0.00016770774,0.000767307,0.0005141341,0.0006985682,0.0008269154,0.0007841678,0.0010157533,0.00014756073],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00091667526,0.0004909757,0.3011885,0.00011726372,0.00069875974,0.0001923001,0.00018436828,0.5544205,0.010698169,0.0043278625,0.004405806,0.12235879],"study_design_scores_gemma":[0.0000075646335,0.00002256998,0.010044979,0.0000025138359,0.000011231719,0.000005582286,0.000020395393,0.9884552,0.0006475282,0.00070046616,0.00007851619,0.000003455305],"about_ca_topic_score_codex":0.012129844,"about_ca_topic_score_gemma":0.007110489,"teacher_disagreement_score":0.012129844,"about_ca_system_score_codex":0.0006763036,"about_ca_system_score_gemma":0.0007878664,"threshold_uncertainty_score":0.024118483},"labels":[],"label_agreement":null},{"id":"W4205455636","doi":"10.1029/2021jb023060","title":"The Rise, Peak and Decline of the Seismic Hazard Related to Hydraulic Fracturing Activities in the Duvernay Play, Fox Creek Area, Alberta","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta; Alberta Energy","funders":"","keywords":"Induced seismicity; Seismic hazard; Hydraulic fracturing; Seismology; Geology; Maximum magnitude; Magnitude (astronomy); Hazard; Seismic risk; Geotechnical engineering","score_opus":0.02540457904909806,"score_gpt":0.2925095162745289,"score_spread":0.2671049372254309,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4205455636","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99684566,0.00012027531,0.00014608713,0.00008020741,0.0000025162685,0.000008448229,0.0009016959,0.000011699565,0.0018833991],"genre_scores_gemma":[0.9975198,0.00009675357,0.00012992304,0.000013496535,0.0000016763064,0.0000033356605,0.00055544823,0.00000204699,0.0016774972],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981874,0.000010056551,0.0000060632083,0.00002777847,0.000073145566,0.00006413085],"domain_scores_gemma":[0.99951947,0.000048818154,0.0000908562,0.000014372605,0.000199238,0.00012716561],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018984573,0.00018817814,0.00012312284,0.0012880457,0.0005779463,0.0007776631,0.0005507943,0.0002590372,0.0016188602],"category_scores_gemma":[0.0007453574,0.00013000653,0.00017515836,0.0012671744,0.0006562849,0.00018200406,0.00046624415,0.00017543785,0.00012729404],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008838127,0.000022464532,0.9855735,0.00002270962,0.000042043543,0.00025319715,0.00080030813,0.0024317743,0.0017797401,0.00031449168,0.0008074955,0.007863861],"study_design_scores_gemma":[0.0000020884258,0.000009748584,0.9973901,0.0000057241837,0.0000052375394,0.000023892244,0.0008386619,0.00090234453,0.00008320401,0.000022831386,0.00071213185,0.000004142919],"about_ca_topic_score_codex":0.9655159,"about_ca_topic_score_gemma":0.98849046,"teacher_disagreement_score":0.03448409,"about_ca_system_score_codex":0.008458895,"about_ca_system_score_gemma":0.0057156407,"threshold_uncertainty_score":0.06937426},"labels":[],"label_agreement":null},{"id":"W4206689009","doi":"10.1029/2021jb022352","title":"Listvenite Formation During Mass Transfer into the Leading Edge of the Mantle Wedge: Initial Results from Oman Drilling Project Hole BT1B","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; University of Calgary","funders":"Japan Agency for Marine-Earth Science and Technology; Natural Environment Research Council; Japan Society for the Promotion of Science; NASA Astrobiology Institute; Alfred P. Sloan Foundation; Deutsche Forschungsgemeinschaft; Sight Research UK; National Science Foundation","keywords":"Geology; Peridotite; Subduction; Ophiolite; Geochemistry; Mantle (geology); Mantle wedge; Metamorphic rock; Accretionary wedge; Metamorphic core complex; Lithosphere; Petrology; Tectonics; Seismology; Extensional definition","score_opus":0.045308561205128786,"score_gpt":0.30032675944444326,"score_spread":0.2550181982393145,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4206689009","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99772984,0.00019997999,0.00022010769,0.000013379769,0.0000027123713,0.000013115377,0.0005498572,0.000014709271,0.0012562558],"genre_scores_gemma":[0.9982685,0.00013128322,0.00047572376,0.000010886829,0.0000026272962,0.00001257347,0.00043192774,0.000010017066,0.0006564162],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998191,0.000017919765,0.00000945667,0.000040270475,0.000055202505,0.000058110225],"domain_scores_gemma":[0.9998636,0.000020267209,0.000042587464,0.000013979448,0.00004482673,0.000014697804],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029837972,0.00056070543,0.00033489775,0.0014555161,0.0008487335,0.000692781,0.0003229638,0.00045668078,0.0009822142],"category_scores_gemma":[0.0003194712,0.00026058665,0.0002306569,0.0011629355,0.00043753354,0.0004265682,0.00053331984,0.00021440577,0.00029233893],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001224532,0.0002569553,0.7817773,0.00035923018,0.00010368131,0.0023754786,0.0038296455,0.0022550242,0.15432957,0.00032808934,0.0005520994,0.05260843],"study_design_scores_gemma":[0.000016087752,0.00015470297,0.9771877,0.00002931319,0.000040747826,0.00030993737,0.0009328635,0.0011089017,0.016819336,0.000074420306,0.003314358,0.000011760804],"about_ca_topic_score_codex":0.023479296,"about_ca_topic_score_gemma":0.04560385,"teacher_disagreement_score":0.023479296,"about_ca_system_score_codex":0.00072543597,"about_ca_system_score_gemma":0.00034205776,"threshold_uncertainty_score":0.04668522},"labels":[],"label_agreement":null},{"id":"W4210274574","doi":"10.1029/2021jb022822","title":"Evolution of Short‐Term Seismic Hazard in Alberta, Canada, From Induced and Natural Earthquakes: 2011–2020","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta; Alberta Energy","funders":"","keywords":"Induced seismicity; Seismic hazard; Seismology; Hazard; Natural hazard; Geology; Earthquake scenario; Term (time); Natural (archaeology); Baseline (sea)","score_opus":0.022628172416721788,"score_gpt":0.27387174531162145,"score_spread":0.2512435728948997,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4210274574","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97153723,0.00035481233,0.001377172,0.00039573628,0.000018022396,0.000024184852,0.021989943,0.00014019743,0.004162667],"genre_scores_gemma":[0.9813115,0.00021516754,0.00070130156,0.00003235978,0.000004776428,0.000008366049,0.015541616,0.000009652534,0.0021752862],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999759,0.000014310336,0.000010105847,0.000027365113,0.00013243817,0.000056735855],"domain_scores_gemma":[0.9990682,0.00006109394,0.0001055043,0.00002606406,0.00062134844,0.00011775098],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004734712,0.00035787447,0.00014719198,0.0014000168,0.00045816047,0.0009118041,0.0006053636,0.00034071296,0.0013962574],"category_scores_gemma":[0.001420897,0.00017560956,0.0002933446,0.001760882,0.00030802164,0.0002358858,0.00045549433,0.00029588997,0.00025221246],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042170816,0.000077521145,0.7790923,0.00012005474,0.00023029908,0.00041312588,0.00037730942,0.17551461,0.0019293947,0.0017056118,0.00939973,0.030718291],"study_design_scores_gemma":[0.000016532535,0.000038092214,0.91721,0.00003755114,0.0000410535,0.000086053355,0.00072009856,0.07405192,0.000617764,0.00031902493,0.0068197497,0.000042091557],"about_ca_topic_score_codex":0.9714916,"about_ca_topic_score_gemma":0.98025745,"teacher_disagreement_score":0.028508425,"about_ca_system_score_codex":0.013363112,"about_ca_system_score_gemma":0.011416805,"threshold_uncertainty_score":0.09695661},"labels":[],"label_agreement":null},{"id":"W4210592412","doi":"10.1029/2021jb022100","title":"Ongoing Asthenospheric Upwelling and Delamination‐Style Down‐Welling Beneath Northeast China: Evidence From High‐Resolution Magnetotelluric Profiles","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Geology; Asthenosphere; Lithosphere; Subduction; Magnetotellurics; Crust; Magmatism; Mantle (geology); Upwelling; Oceanic crust; Partial melting; Geochemistry; Geophysics; Petrology; Paleontology; Electrical resistivity and conductivity; Tectonics; Oceanography","score_opus":0.025007961219961888,"score_gpt":0.2577447862743569,"score_spread":0.232736825054395,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4210592412","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995764,0.000027019241,0.000038454895,0.0000066677217,3.8076826e-7,0.0000012951857,0.00013053838,0.000004385093,0.00021501194],"genre_scores_gemma":[0.9996532,0.000025373627,0.00005977917,0.0000025257489,9.4979885e-7,8.870153e-7,0.00017169809,0.0000012279336,0.00008434894],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993145,0.000006304103,0.0000071585014,0.000019961488,0.000016534488,0.000018552342],"domain_scores_gemma":[0.99975866,0.000025993548,0.00008970875,0.0000242008,0.00006531139,0.00003604681],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015878255,0.00021036515,0.00018847047,0.00097576965,0.00034817314,0.000446526,0.00021793744,0.00024003793,0.00051711523],"category_scores_gemma":[0.0002740413,0.00018186113,0.0001630699,0.0011250784,0.00021821917,0.00022408024,0.00023123379,0.000091103706,0.00007794503],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005374663,0.000018552351,0.9710325,0.000022120097,0.00005310532,0.00036248149,0.00069145847,0.0007855385,0.022083364,0.0000544451,0.00007635805,0.0047663315],"study_design_scores_gemma":[0.0000010044794,0.000005029553,0.9987503,0.000001622217,0.0000064507435,0.000022513717,0.0001087121,0.00064092723,0.0003851963,0.000005547096,0.000070692695,0.000001981104],"about_ca_topic_score_codex":0.053357206,"about_ca_topic_score_gemma":0.09067663,"teacher_disagreement_score":0.053357206,"about_ca_system_score_codex":0.00039742427,"about_ca_system_score_gemma":0.00023585522,"threshold_uncertainty_score":0.10609329},"labels":[],"label_agreement":null},{"id":"W4214883837","doi":"10.1029/2021jb022990","title":"Precursory Signal Detected for the 2018 Sierra Negra Volcanic Eruption, Galápagos, Using Seismic Ambient Noise","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; University of Victoria","funders":"","keywords":"Geology; Seismology; Caldera; Sill; Volcano; Magma; Ambient noise level; Induced seismicity; Volcanic hazards; Geomorphology; Petrology; Sound (geography)","score_opus":0.06034327666325191,"score_gpt":0.3213915838203118,"score_spread":0.2610483071570599,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4214883837","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989374,0.000024040957,0.00021633232,0.000012428258,0.0000033756373,0.0000033421088,0.00030667687,0.000024125593,0.0004723375],"genre_scores_gemma":[0.9992549,0.000017094482,0.00019761012,0.0000041150734,0.000005468156,0.0000029881749,0.00041298722,0.000002339755,0.00010249903],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999941,0.0000072208413,0.0000031187938,0.000021908878,0.00001456908,0.000012198872],"domain_scores_gemma":[0.9998374,0.00003184822,0.00004084969,0.0000134002485,0.000040598756,0.000035750665],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000099822886,0.0001925676,0.00011363113,0.00067146786,0.0001262058,0.00027516417,0.00012967967,0.00018043804,0.0004591024],"category_scores_gemma":[0.0005830398,0.00009238236,0.0000836603,0.00039933872,0.000108729655,0.00009852436,0.00025365045,0.00012364735,0.00008472173],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043632838,0.00007128937,0.9301259,0.00004074361,0.00007095255,0.0005695141,0.00040215664,0.0022349367,0.043663997,0.0001307632,0.0004576727,0.021795765],"study_design_scores_gemma":[0.0000047391673,0.000024524148,0.9967449,0.0000024322221,0.000010660594,0.000076949036,0.000060602822,0.001876968,0.00088924204,0.000018994075,0.0002876581,0.0000023643386],"about_ca_topic_score_codex":0.0073072836,"about_ca_topic_score_gemma":0.008878871,"teacher_disagreement_score":0.0073072836,"about_ca_system_score_codex":0.00018129153,"about_ca_system_score_gemma":0.00010299462,"threshold_uncertainty_score":0.014529526},"labels":[],"label_agreement":null},{"id":"W4220710213","doi":"10.1029/2021jb022750","title":"Source Properties of Hydraulic‐Fracturing‐Induced Earthquakes in the Kiskatinaw Area, British Columbia, Canada","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Deutsche Forschungsgemeinschaft","keywords":"Seismology; Geology; Waveform; Hydraulic fracturing; Focal mechanism; Seismic moment; Slip (aerodynamics); Graben; Scaling; Geodesy; Induced seismicity; Geometry; Fault (geology); Geotechnical engineering; Physics; Voltage","score_opus":0.04288432064589042,"score_gpt":0.25769298465045554,"score_spread":0.2148086640045651,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220710213","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9891643,0.00024813405,0.0003683071,0.00007581942,0.000005326157,0.000033076205,0.0059377532,0.000051368224,0.0041158767],"genre_scores_gemma":[0.9939387,0.00020507316,0.00030606642,0.000020612537,0.0000019598358,0.000016398555,0.0033884882,0.000015436208,0.0021072985],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99979085,0.000007690502,0.000014065484,0.00004242959,0.00007535625,0.000069614354],"domain_scores_gemma":[0.9989968,0.00006990541,0.00008719629,0.000039594423,0.00068218523,0.00012439901],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017359694,0.0003826846,0.0002708748,0.0023382818,0.0016661746,0.0011817134,0.00084224984,0.0002993819,0.0026663279],"category_scores_gemma":[0.0011349963,0.00023125364,0.00021568808,0.004606473,0.00041953608,0.00027152637,0.00062998163,0.00028278554,0.00041165084],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000119298114,0.00004990831,0.9516721,0.00012211426,0.00014108648,0.0005897673,0.0015177731,0.0045377444,0.006631796,0.00026872352,0.0029351658,0.031414464],"study_design_scores_gemma":[0.0000076192455,0.00000508753,0.9948054,0.000022737106,0.000022888222,0.00006244002,0.0011604127,0.002030266,0.00038842406,0.000025065212,0.0014515934,0.000018105591],"about_ca_topic_score_codex":0.9934934,"about_ca_topic_score_gemma":0.9969531,"teacher_disagreement_score":0.0118232835,"about_ca_system_score_codex":0.0118232835,"about_ca_system_score_gemma":0.010217679,"threshold_uncertainty_score":0.085784316},"labels":[],"label_agreement":null},{"id":"W4220717363","doi":"10.1029/2021jb022334","title":"Active and Passive Seismic Imaging of the Central Abitibi Greenstone Belt, Larder Lake, Ontario","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Laurentian University","funders":"Canada First Research Excellence Fund","keywords":"Geology; Receiver function; Seismology; Passive seismic; Greenstone belt; Archean; Shear zone; Seismic anisotropy; Crust; Mafic; Seismic refraction; Petrology; Geophysics; Mantle (geology); Geochemistry; Tectonics; Lithosphere","score_opus":0.017896269869089,"score_gpt":0.26782539689154977,"score_spread":0.24992912702246078,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220717363","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9939494,0.00009993108,0.0003046745,0.00005871637,0.0000020611728,0.000026620839,0.000960702,0.00003817367,0.0045597954],"genre_scores_gemma":[0.9944338,0.00010775139,0.00088323146,0.000022573427,0.000002645248,0.0000204534,0.00069954165,0.000008520418,0.0038214903],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987054,0.0000050700132,0.0000041598814,0.000027465536,0.00005209598,0.0000406507],"domain_scores_gemma":[0.999798,0.000011501748,0.000029956342,0.000007893315,0.000115156705,0.00003759826],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009785817,0.00021159464,0.00013436683,0.0013181895,0.00089529564,0.00066525995,0.00040281573,0.00019107989,0.001301046],"category_scores_gemma":[0.0003042412,0.00019454176,0.000077538025,0.0012344398,0.00042923304,0.00017880328,0.00047335343,0.00009870557,0.0002577114],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003609843,0.0000862407,0.7804601,0.0001875085,0.00007086738,0.0009356994,0.0068099713,0.002174551,0.1331809,0.00088351965,0.0028701664,0.071979396],"study_design_scores_gemma":[0.000017038568,0.000026079166,0.9922416,0.000014066856,0.000013299067,0.00006352543,0.001420909,0.0014160004,0.0014276311,0.00003391262,0.0033186201,0.000007267785],"about_ca_topic_score_codex":0.91932034,"about_ca_topic_score_gemma":0.987773,"teacher_disagreement_score":0.080679655,"about_ca_system_score_codex":0.004540337,"about_ca_system_score_gemma":0.0038791902,"threshold_uncertainty_score":0.16230953},"labels":[],"label_agreement":null},{"id":"W4220799416","doi":"10.1029/2021jb022825","title":"Pair Selection Optimization for InSAR Time Series Processing","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Synthetic Aperture Radar (SAR) Applications and Techniques","field":"Engineering","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"Belgian Federal Science Policy Office","keywords":"Interferometric synthetic aperture radar; Synthetic aperture radar; Computer science; Interferometry; Remote sensing; Algorithm; Time series; Artificial intelligence; Geology; Data mining; Machine learning","score_opus":0.0180282708526234,"score_gpt":0.30194053081620326,"score_spread":0.2839122599635798,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220799416","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.025352707,0.00024947224,0.9714494,0.00014816759,0.00006673846,0.00006994977,0.00021089971,0.00095571444,0.0014970248],"genre_scores_gemma":[0.42717916,0.00021201742,0.56478626,0.00018531487,0.00018080966,0.00041594804,0.0018769942,0.00054622395,0.0046172882],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9988335,0.0005528861,0.000045064757,0.00022423994,0.00023950964,0.00010491559],"domain_scores_gemma":[0.9982627,0.0012050522,0.00010055462,0.000116425894,0.00024945344,0.00006586004],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001317582,0.0017271108,0.0012129106,0.0013195687,0.0005353359,0.0010041771,0.0011259136,0.00094725296,0.0062470906],"category_scores_gemma":[0.0035329438,0.00054939697,0.0010621474,0.0015872559,0.00054606487,0.00083601504,0.0010336727,0.0010585261,0.0014549181],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031571265,0.00018913318,0.001527935,0.00014557365,0.00016603753,0.0002032335,0.00007071826,0.8071931,0.0049635665,0.005953511,0.006266421,0.1730051],"study_design_scores_gemma":[0.000010529094,0.000029379013,0.00024980734,0.0000029869439,0.000010513531,0.0000135551145,0.000012055249,0.9963953,0.00073005585,0.0019967756,0.0005449799,0.0000041650624],"about_ca_topic_score_codex":0.0029250835,"about_ca_topic_score_gemma":0.0025243054,"teacher_disagreement_score":0.0062470906,"about_ca_system_score_codex":0.0005618637,"about_ca_system_score_gemma":0.0008348111,"threshold_uncertainty_score":0.02089864},"labels":[],"label_agreement":null},{"id":"W4220807159","doi":"10.1029/2021jb023631","title":"Influence of 3D Earth Structure on Glacial Isostatic Adjustment in the Russian Arctic","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Russian Science Foundation; Ministry of Education - Singapore; National Research Foundation Singapore","keywords":"Post-glacial rebound; Deglaciation; Lithosphere; Geology; Arctic; Mantle (geology); Last Glacial Maximum; Ice sheet; Sea level; Glacial period; Physical geography; Oceanography; Geophysics; Paleontology; Geography; Tectonics","score_opus":0.025126151272997607,"score_gpt":0.31546635339439694,"score_spread":0.2903402021213993,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220807159","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967769,0.00006440549,0.0019037202,0.000042252737,0.0000067807055,0.000005184257,0.00041870342,0.00008690708,0.000695073],"genre_scores_gemma":[0.99897826,0.00002577246,0.00049391354,0.000008098342,0.0000019472363,0.000004257847,0.00038581697,0.000017515304,0.000084586725],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9997869,0.0000723462,0.000014666517,0.00006926786,0.00002441392,0.000032403674],"domain_scores_gemma":[0.99960476,0.00015318685,0.00006677224,0.00007438156,0.0000662168,0.000034674395],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005615952,0.00048708273,0.00046010912,0.0005872653,0.0003919405,0.0011429715,0.0005525089,0.00052212155,0.00068805675],"category_scores_gemma":[0.0015015826,0.00040880937,0.0012497087,0.00043519516,0.0005022778,0.0003870416,0.0006395894,0.00024983587,0.00023031296],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008819257,0.000026239362,0.08738105,0.000022180271,0.0002187933,0.00009331165,0.00008546882,0.90485466,0.0033851482,0.00031466776,0.00015391785,0.0033763687],"study_design_scores_gemma":[0.000030524934,0.000038196584,0.08946716,0.000013759125,0.00007040538,0.000049121027,0.00007838132,0.90836585,0.0010699679,0.0002806456,0.00049881655,0.000037172143],"about_ca_topic_score_codex":0.07866632,"about_ca_topic_score_gemma":0.040967513,"teacher_disagreement_score":0.07866632,"about_ca_system_score_codex":0.0008325018,"about_ca_system_score_gemma":0.0007352953,"threshold_uncertainty_score":0.1564169},"labels":[],"label_agreement":null},{"id":"W4220837062","doi":"10.1029/2021jb023097","title":"Understanding the Geodetic Signature of Large Aquifer Systems: Example of the Ozark Plateaus in Central United States","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; Institut de Physique du Globe de Paris; Office for Science and Technology of the Embassy of France in the United States","keywords":"Poromechanics; Aquifer; Geology; Groundwater; Geodetic datum; Piezometer; Aquifer properties; Deformation (meteorology); Pore water pressure; Soil science; Geotechnical engineering; Geophysics; Geodesy; Groundwater recharge; Porous medium","score_opus":0.1169437691721006,"score_gpt":0.30786133152362827,"score_spread":0.19091756235152768,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220837062","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985864,0.000049306946,0.00020222383,0.000044863456,0.0000012682752,0.0000052814225,0.00046762172,0.00001275319,0.0006301877],"genre_scores_gemma":[0.9990922,0.000027148151,0.00037356224,0.000008115294,0.000001936722,0.0000038029195,0.00039759805,0.0000022457136,0.000093345145],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999269,0.000008437956,0.0000063697285,0.000021096026,0.000015299665,0.000021936208],"domain_scores_gemma":[0.99981123,0.000027733635,0.00004237574,0.00001646646,0.0000734741,0.000028735247],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015376709,0.00014565534,0.00014679448,0.0014097167,0.0004136833,0.0005314202,0.0002260252,0.0002658407,0.0006165116],"category_scores_gemma":[0.00032925094,0.000072475166,0.000118049706,0.0024748389,0.00032493856,0.00023943972,0.00055629935,0.00012679795,0.000054544318],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000083733146,0.0000621049,0.95795774,0.000037110814,0.000042562246,0.000755185,0.0009109605,0.00430225,0.009112864,0.00036823194,0.00078214373,0.025585143],"study_design_scores_gemma":[0.0000027786818,0.000006756239,0.99401796,0.000004628971,0.0000073588258,0.000032229447,0.00097382074,0.004254519,0.00024180894,0.000057136425,0.0003965377,0.0000045094503],"about_ca_topic_score_codex":0.20955053,"about_ca_topic_score_gemma":0.4253405,"teacher_disagreement_score":0.20955053,"about_ca_system_score_codex":0.0005257234,"about_ca_system_score_gemma":0.00046933847,"threshold_uncertainty_score":0.41666162},"labels":[],"label_agreement":null},{"id":"W4220837374","doi":"10.1029/2021jb023046","title":"Magmatism at Passive Margins: Effects of Depth‐Dependent Wide Rifting and Lithospheric Counterflow","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Total","keywords":"Magmatism; Geology; Lithosphere; Rift; Crust; Mantle (geology); Continental crust; Continental margin; Large igneous province; Passive margin; Petrology; Geophysics; Seismology; Tectonics","score_opus":0.0138022630987953,"score_gpt":0.25884768931953306,"score_spread":0.24504542622073777,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220837374","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983961,0.00005735181,0.0005854477,0.000045098408,0.0000043117475,0.000004879415,0.000077709854,0.000022917753,0.00080621924],"genre_scores_gemma":[0.999736,0.00002256542,0.000099906574,0.0000052005303,0.0000011925455,0.0000020200744,0.000020069947,0.0000028920892,0.000110101064],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99988616,0.000034578705,0.000008535916,0.000024873658,0.000013681458,0.00003213664],"domain_scores_gemma":[0.9994448,0.00025343825,0.0001242994,0.000041971878,0.000040922023,0.00009465475],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025734995,0.0005347089,0.00032009496,0.00036910214,0.00027016626,0.0008212834,0.0004995203,0.00066025776,0.00124383],"category_scores_gemma":[0.0014439091,0.00035416617,0.00063486386,0.00020801296,0.0006529749,0.00055931177,0.00074767123,0.0004306749,0.00007646176],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003148954,0.00012776924,0.07186166,0.000069242844,0.00017730547,0.0002712873,0.00008615275,0.88506734,0.038537953,0.0009682891,0.00014201817,0.002375982],"study_design_scores_gemma":[0.0000780695,0.00019783546,0.061792687,0.000012054111,0.00009652329,0.00006773229,0.000086526554,0.93141246,0.0055896756,0.00038930099,0.00025137104,0.000025815001],"about_ca_topic_score_codex":0.02142327,"about_ca_topic_score_gemma":0.009817013,"teacher_disagreement_score":0.02142327,"about_ca_system_score_codex":0.0008648035,"about_ca_system_score_gemma":0.00052898284,"threshold_uncertainty_score":0.042597175},"labels":[],"label_agreement":null},{"id":"W4220933785","doi":"10.1029/2021jb022480","title":"Magnitude‐Frequency Distributions and Slip‐History Predictions for Earthquakes Using Cellular Automata and Absorbing Markov Chains","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; University of Alberta","funders":"","keywords":"Statistical physics; Slip (aerodynamics); Markov chain; Cellular automaton; Scaling; Markov chain Monte Carlo; Discretization; Markov process; Dissipation; Probability distribution; Series (stratigraphy); Mathematics; Monte Carlo method; Computer science; Physics; Statistics; Algorithm; Geology; Mathematical analysis; Geometry","score_opus":0.06157333613192281,"score_gpt":0.3058741097551804,"score_spread":0.2443007736232576,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220933785","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7021911,0.000115342475,0.29380456,0.0002767624,0.000023634382,0.000028573097,0.00019357647,0.00021680426,0.0031497097],"genre_scores_gemma":[0.9965383,0.000028973018,0.0030344245,0.0000072499306,0.0000054974653,0.000013612586,0.000043151806,0.000008098062,0.00032075788],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998715,0.000036720925,0.000008649216,0.000029522445,0.000029584085,0.000024013758],"domain_scores_gemma":[0.9973807,0.0019344436,0.00027949933,0.00010728144,0.00022131125,0.00007673978],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000663544,0.00024434042,0.00026344723,0.0006776145,0.00031543057,0.0005935755,0.0005119021,0.00048485555,0.0010562948],"category_scores_gemma":[0.0048251813,0.00026410687,0.0003496822,0.00036642657,0.0006588425,0.0006678728,0.0002843498,0.00042045454,0.00011068008],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001389463,0.000012737559,0.002827589,0.000006252906,0.000006661455,0.000027066333,0.000030527943,0.983417,0.0005879098,0.011214507,0.000108591885,0.0017472648],"study_design_scores_gemma":[6.5828846e-7,0.0000015487783,0.0001841756,8.168956e-7,6.5880596e-7,0.0000020639359,0.0000021366618,0.99814117,0.00006064837,0.0015891829,0.000015701082,0.0000011834907],"about_ca_topic_score_codex":0.012399785,"about_ca_topic_score_gemma":0.008120756,"teacher_disagreement_score":0.012399785,"about_ca_system_score_codex":0.0009196251,"about_ca_system_score_gemma":0.00057788624,"threshold_uncertainty_score":0.024655223},"labels":[],"label_agreement":null},{"id":"W4221134092","doi":"10.1029/2021jb022704","title":"Deep Sourced Fluids for Peridotite Carbonation in the Shallow Mantle Wedge of a Fossil Subduction Zone: Sr and C Isotope Profiles of OmanDP Hole BT1B","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Japan Society for the Promotion of Science; Japan Agency for Marine-Earth Science and Technology; Natural Environment Research Council; Lamont-Doherty Earth Observatory, Columbia University; Centre National de la Recherche Scientifique; Sultan Qaboos University; Sight Research UK; Deutsche Forschungsgemeinschaft; Alfred P. Sloan Foundation; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; Canada First Research Excellence Fund; National Aeronautics and Space Administration; University of Southampton; University of Calgary; National Science Foundation","keywords":"Peridotite; Ophiolite; Geology; Geochemistry; Mantle (geology); Mantle wedge; Radiogenic nuclide; Subduction; Outcrop; Paleontology; Tectonics","score_opus":0.02969656789824447,"score_gpt":0.2875738292092215,"score_spread":0.257877261310977,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4221134092","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999435,0.00003706153,0.00003097711,0.000004729235,5.6939444e-7,0.0000010102777,0.00018931513,0.0000048326347,0.0002963999],"genre_scores_gemma":[0.99929285,0.000029081823,0.00007092807,0.0000043280183,0.0000011736349,0.000002368322,0.00031491028,0.0000049981786,0.00027931642],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995124,0.000002662813,0.0000028146642,0.0000151034255,0.000011651205,0.000016469017],"domain_scores_gemma":[0.99994016,0.0000070243236,0.000017354838,0.0000043904806,0.000015850599,0.000015162038],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007389612,0.0002803264,0.00016433519,0.0011247805,0.00043376506,0.0005926478,0.00021450125,0.00027690112,0.0010722976],"category_scores_gemma":[0.00014796722,0.00016579911,0.00011133732,0.0005731037,0.00025160672,0.000294002,0.00033612837,0.00014197381,0.00021184962],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042882684,0.000049108323,0.8100658,0.000043657776,0.000044801825,0.0003885559,0.0009847785,0.0003500465,0.17708962,0.00011742148,0.00012225573,0.010315078],"study_design_scores_gemma":[0.0000040155605,0.000019062527,0.99651897,0.0000031231314,0.000005410943,0.0000599719,0.00016801321,0.00026326228,0.0026898093,0.000010321614,0.0002560948,0.0000019650586],"about_ca_topic_score_codex":0.018793797,"about_ca_topic_score_gemma":0.018453242,"teacher_disagreement_score":0.018793797,"about_ca_system_score_codex":0.0004232829,"about_ca_system_score_gemma":0.00015419802,"threshold_uncertainty_score":0.037368774},"labels":[],"label_agreement":null},{"id":"W4225003216","doi":"10.1029/2022jb024091","title":"Multistage Nucleation of the 2021 Yangbi M<sub>S</sub> 6.4 Earthquake, Yunnan, China and Its Foreshocks","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Natural Science Foundation of China","keywords":"Foreshock; Seismology; Geology; Nucleation; Slip (aerodynamics); Fault (geology); Aftershock; Physics","score_opus":0.02676441118395927,"score_gpt":0.27962201763087796,"score_spread":0.2528576064469187,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4225003216","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99944407,0.0000441034,0.00021052275,0.0000051800125,0.0000019154554,0.0000075453167,0.00013196825,0.0000066470693,0.00014796708],"genre_scores_gemma":[0.9990964,0.000029640674,0.00021136912,0.0000021976039,0.0000033760489,0.0000068841446,0.00048840715,0.0000013908815,0.00016039604],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999014,0.0000061580013,0.0000071842337,0.000028620641,0.000026044956,0.00003050431],"domain_scores_gemma":[0.9996965,0.000022375012,0.00011648021,0.000023898123,0.000050521114,0.00009027852],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020375154,0.00024024007,0.0002680276,0.001175528,0.00044833974,0.00033225247,0.00033324352,0.00019514648,0.0004899169],"category_scores_gemma":[0.0004364754,0.0001931929,0.00022463342,0.0008797357,0.00016143048,0.0002160248,0.0003889778,0.00012628887,0.000103821054],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017406617,0.000042783697,0.9549454,0.000054540807,0.000057836012,0.0011111517,0.00040990583,0.0041610333,0.025553966,0.00020571967,0.0003619972,0.012921566],"study_design_scores_gemma":[0.0000034119257,0.000026172282,0.9948106,0.0000025146735,0.000010531313,0.00006302376,0.00009275234,0.0035507747,0.0011476205,0.000032729145,0.000254618,0.000005257951],"about_ca_topic_score_codex":0.018186772,"about_ca_topic_score_gemma":0.027947035,"teacher_disagreement_score":0.018186772,"about_ca_system_score_codex":0.000464728,"about_ca_system_score_gemma":0.0004385913,"threshold_uncertainty_score":0.03616184},"labels":[],"label_agreement":null},{"id":"W4225082363","doi":"10.1029/2021jb023599","title":"Random Forest Predictions of Fine Ash Concentration and Charging Processes From Experimentally Generated Volcanic Discharges","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Lightning and Electromagnetic Phenomena","field":"Physics and Astronomy","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Mechanics; Volcanic ash; Particle (ecology); Atmospheric sciences; Plume; Volcano; Meteorology; Environmental science; Chemistry; Mineralogy; Geology; Physics; Seismology","score_opus":0.018591484758200088,"score_gpt":0.29574481891855986,"score_spread":0.27715333416035975,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4225082363","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.91048324,0.00017775464,0.086481474,0.000161998,0.000037101185,0.00005637161,0.0007598543,0.0008061223,0.001035994],"genre_scores_gemma":[0.9849305,0.00003130017,0.01332809,0.000031635707,0.000010908856,0.000045134053,0.0011625016,0.00002865496,0.00043125145],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998565,0.00003879099,0.000005779083,0.000042026066,0.000019417512,0.000037496542],"domain_scores_gemma":[0.9982401,0.0011820672,0.000109250905,0.000070203474,0.00032431495,0.000074122356],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012010805,0.00073476083,0.00036312258,0.0004439707,0.00029732336,0.00030564278,0.00062098226,0.00078037125,0.0011698562],"category_scores_gemma":[0.0033300363,0.00019408044,0.0006226654,0.0002326134,0.00029884122,0.00038649203,0.00022270899,0.0006916302,0.000368564],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006754803,0.00005600596,0.006928568,0.0000150539745,0.000014949051,0.000017466431,0.0000075361054,0.98368376,0.0009867898,0.00019127833,0.00026407943,0.0077669676],"study_design_scores_gemma":[0.0000034042355,0.000010154962,0.0006051241,0.0000016195311,0.0000013931345,0.0000025831507,0.0000017532026,0.9989784,0.00027718686,0.00009417803,0.000022595957,0.0000015713539],"about_ca_topic_score_codex":0.012975327,"about_ca_topic_score_gemma":0.009419274,"teacher_disagreement_score":0.012975327,"about_ca_system_score_codex":0.00048499883,"about_ca_system_score_gemma":0.0005279394,"threshold_uncertainty_score":0.025799632},"labels":[],"label_agreement":null},{"id":"W4225625002","doi":"10.1029/2021jb022878","title":"Time‐Lapse Record of an Earthquake in the Dry Felsic Lower Continental Crust Preserved in a Pseudotachylyte‐Bearing Fault","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"","keywords":"Geology; Continental crust; Felsic; Quartz; Granulite; Ilmenite; Mylonite; Shear zone; Feldspar; Crust; Slip (aerodynamics); Petrology; Geochemistry; Mineralogy; Seismology; Mafic; Tectonics; Geomorphology","score_opus":0.03980202957972251,"score_gpt":0.30695919499104257,"score_spread":0.26715716541132006,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4225625002","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999132,0.000040515326,0.00008880692,0.0000047702515,9.686253e-7,0.0000027391054,0.00029841822,0.000007180869,0.00042472436],"genre_scores_gemma":[0.99901617,0.000027344493,0.00013571813,0.0000037392726,0.000003691767,0.0000029718717,0.00059568527,0.0000025860559,0.0002121401],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997234,0.0000019517004,0.0000020250352,0.000009131523,0.0000062209497,0.000008390976],"domain_scores_gemma":[0.99985766,0.000012325433,0.000049220598,0.000013484,0.000031428626,0.000035830988],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008730721,0.00010969933,0.0001354518,0.0009529885,0.00029762796,0.00023354634,0.00016918975,0.00021365703,0.0008899639],"category_scores_gemma":[0.00018797729,0.000100899335,0.00009748273,0.0005681382,0.00020677963,0.000117659525,0.00029850466,0.00013807636,0.0002490888],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035882587,0.000088399465,0.7335539,0.00006317613,0.00009557277,0.0009303118,0.0010146876,0.00051077077,0.24909,0.00015257737,0.00030337198,0.0138384085],"study_design_scores_gemma":[0.0000012966885,0.000028410215,0.99856645,0.0000015023298,0.0000059003714,0.00009742891,0.00004395064,0.00015711,0.00084409094,0.0000056827853,0.00024674338,0.0000014641747],"about_ca_topic_score_codex":0.00522688,"about_ca_topic_score_gemma":0.013176104,"teacher_disagreement_score":0.00522688,"about_ca_system_score_codex":0.00021932117,"about_ca_system_score_gemma":0.000063488886,"threshold_uncertainty_score":0.010392904},"labels":[],"label_agreement":null},{"id":"W4225667776","doi":"10.1029/2021jb023246","title":"Crustal Structure Beneath the Northern Appalachians and the Eastern Grenville Province","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Terrane; Crust; Proterozoic; Paleontology; Seismology; Archean; Tectonics; Continental crust","score_opus":0.016133825253729885,"score_gpt":0.2594099402315069,"score_spread":0.24327611497777699,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4225667776","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973947,0.00013526712,0.000047322657,0.000030014577,0.0000018368822,0.00000434418,0.0005302247,0.000011521448,0.0018448835],"genre_scores_gemma":[0.9989298,0.00005713336,0.00010624042,0.000008264466,9.743545e-7,0.0000029205294,0.0005166432,0.0000026556165,0.00037531933],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983156,0.00001039496,0.000013742759,0.000051120816,0.000035999765,0.00005724173],"domain_scores_gemma":[0.9997286,0.00002399975,0.00007094722,0.000019532064,0.00011673484,0.00004009501],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001473348,0.0003272166,0.00020107279,0.0015634007,0.00057841884,0.000960491,0.0005037683,0.0002690835,0.001661995],"category_scores_gemma":[0.00050692284,0.0001446247,0.00022123406,0.0011892805,0.00042488013,0.00027651884,0.0006464096,0.0001811557,0.00025529834],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000072982955,0.000016750244,0.9749116,0.000037407524,0.00006232035,0.0004463214,0.0007688482,0.0013487313,0.011008491,0.00016781078,0.0002896089,0.010869079],"study_design_scores_gemma":[0.000001437892,0.0000037609213,0.9986297,0.000010547424,0.0000064854985,0.000042605225,0.00043379955,0.00042340078,0.00014162436,0.000013322642,0.0002891226,0.0000042622514],"about_ca_topic_score_codex":0.75147676,"about_ca_topic_score_gemma":0.8839671,"teacher_disagreement_score":0.75147676,"about_ca_system_score_codex":0.001621106,"about_ca_system_score_gemma":0.0016987248,"threshold_uncertainty_score":0.49997365},"labels":[],"label_agreement":null},{"id":"W4225686858","doi":"10.1029/2021jb023519","title":"Community‐Driven Code Comparisons for Three‐Dimensional Dynamic Modeling of Sequences of Earthquakes and Aseismic Slip","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":73,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"High Performance Research Computing, Texas A and M University; Natural Sciences and Engineering Research Council of Canada; U.S. Geological Survey; European Commission; Nederlandse Organisatie voor Wetenschappelijk Onderzoek; Japan Society for the Promotion of Science; Southern California Earthquake Center; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; National Science Foundation","keywords":"Slip (aerodynamics); Observable; Finite element method; Geology; Earthquake rupture; Seismology; Computer science; Mechanics; Physics; Fault (geology); Structural engineering; Engineering","score_opus":0.09982133201517948,"score_gpt":0.3492980179679504,"score_spread":0.24947668595277092,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4225686858","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9689322,0.00019542637,0.015157536,0.000266072,0.00013793856,0.0002109978,0.0022054578,0.0027956893,0.010098685],"genre_scores_gemma":[0.96527404,0.00009504537,0.026932273,0.0001096399,0.000017942262,0.00034942152,0.0053847535,0.0008053102,0.001031473],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9986773,0.00041073453,0.00013810386,0.00018519437,0.0004225301,0.00016609931],"domain_scores_gemma":[0.99371225,0.002217,0.00028117592,0.0010311215,0.0023224663,0.00043588315],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0037157536,0.0008071701,0.00051940215,0.0011822837,0.0007271535,0.0008730819,0.002319526,0.0013400913,0.0021854318],"category_scores_gemma":[0.008869159,0.00035062808,0.0008693695,0.0010116416,0.0006479112,0.0011627149,0.001696446,0.001144831,0.00055481424],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010756939,0.0022240367,0.038704667,0.00036588783,0.00024436085,0.00027496877,0.00046314218,0.8804521,0.013501048,0.008198282,0.008865791,0.045630027],"study_design_scores_gemma":[0.00019247516,0.0003794471,0.005020565,0.000028186243,0.000020390074,0.000031131025,0.00014561745,0.9849834,0.0058000176,0.0011291003,0.0022332268,0.00003640961],"about_ca_topic_score_codex":0.011472295,"about_ca_topic_score_gemma":0.012297137,"teacher_disagreement_score":0.011472295,"about_ca_system_score_codex":0.0009340401,"about_ca_system_score_gemma":0.0016303741,"threshold_uncertainty_score":0.022810996},"labels":[],"label_agreement":null},{"id":"W4226087893","doi":"10.1029/2022jb024501","title":"Thank You to Our 2021 Peer Reviewers","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geotourism and Geoheritage Conservation","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Peer review; Psychology; Political science; Law","score_opus":0.0634556101875477,"score_gpt":0.34588515233589767,"score_spread":0.28242954214835,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4226087893","genre_codex":"editorial","genre_gemma":"editorial","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"editorial","genre_consensus":"editorial","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0011844712,0.011777348,0.005260412,0.2944717,0.65457,0.0007221026,0.0030703777,0.0038018906,0.025141716],"genre_scores_gemma":[0.012666851,0.013898886,0.015463776,0.14669842,0.32032865,0.0015962801,0.004966291,0.0070576887,0.47732317],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9778922,0.004809116,0.001998065,0.002993454,0.011328957,0.0009780935],"domain_scores_gemma":[0.5508381,0.012424024,0.010888131,0.009408022,0.39120728,0.025234487],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0174068,0.0018947563,0.0024817442,0.0044962238,0.004824968,0.016060125,0.002838185,0.0046647443,0.146737],"category_scores_gemma":[0.1857066,0.0009832096,0.0014470974,0.0029077136,0.0017769032,0.007632217,0.0049501415,0.0072965613,0.22661257],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001446876,0.000005044272,0.00013962438,0.000064496824,0.000004933374,0.000056434605,0.00006484603,0.000014365778,0.00009429734,0.00013705509,0.98778695,0.011617393],"study_design_scores_gemma":[0.000011057075,0.000008566413,0.00033499242,0.00009933959,0.000009810545,0.00013913264,0.00029818836,0.000055509117,0.00010440189,0.00046142755,0.99844897,0.000028751787],"about_ca_topic_score_codex":0.004964916,"about_ca_topic_score_gemma":0.011895082,"teacher_disagreement_score":0.146737,"about_ca_system_score_codex":0.0022391363,"about_ca_system_score_gemma":0.009396468,"threshold_uncertainty_score":0.49088413},"labels":[],"label_agreement":null},{"id":"W4226289444","doi":"10.1029/2022jb024131","title":"1.2 Myr Band of Earth‐Mars Obliquity Modulation on the Evolution of Cold Late Miocene to Warm Early Pliocene Climate","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Geology; Aridification; Global cooling; Paleontology; Late Miocene; myr; Paleoclimatology; Glacial period; Cenozoic; Climate change; East Asian Monsoon; Neogene; Climatology; Northern Hemisphere; Monsoon; Oceanography","score_opus":0.03919182855085103,"score_gpt":0.3116214996570614,"score_spread":0.27242967110621036,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4226289444","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987662,0.00003499014,0.00009179512,0.00002536647,0.000002081871,0.0000014454956,0.00017910125,0.0000117899235,0.0008873925],"genre_scores_gemma":[0.99974364,0.000012731651,0.000025794445,0.000003468889,0.0000017892772,9.744995e-7,0.000087234446,0.0000025359798,0.000121950055],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99997485,0.0000049325963,0.0000011460359,0.000007983124,0.0000033137023,0.000007672612],"domain_scores_gemma":[0.999905,0.00001682737,0.00003584003,0.000010500605,0.000014854025,0.000016914315],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009149609,0.00012848819,0.0000873073,0.00036102207,0.00017643432,0.00026026682,0.000093157476,0.00012546893,0.0023856063],"category_scores_gemma":[0.00036636597,0.0000830344,0.00007631694,0.00018083781,0.00018544859,0.00010583439,0.00026561494,0.00015037702,0.00021207434],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044586594,0.000031114574,0.86933815,0.0000365308,0.00006841104,0.00024881205,0.00060598686,0.0026222772,0.10901687,0.00046929077,0.0006459989,0.01647067],"study_design_scores_gemma":[0.0000027623728,0.0000202332,0.9981572,0.0000018182703,0.0000042766073,0.000033838023,0.00003914808,0.00050831685,0.00081425917,0.00002996768,0.000386402,0.0000018855773],"about_ca_topic_score_codex":0.0018133741,"about_ca_topic_score_gemma":0.003855726,"teacher_disagreement_score":0.0023856063,"about_ca_system_score_codex":0.00015118098,"about_ca_system_score_gemma":0.000062377214,"threshold_uncertainty_score":0.007980704},"labels":[],"label_agreement":null},{"id":"W4281618614","doi":"10.1029/2021jb023681","title":"Understanding the Anisotropic Mechanical Behavior of Single‐Crystalline Alpha Quartz From the Insight of Molecular Dynamics","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-Velocity Impact and Material Behavior","field":"Materials Science","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Stantec (Canada)","funders":"","keywords":"Quartz; Anisotropy; Materials science; Molecular dynamics; Strain rate; Stress (linguistics); Uniaxial tension; Composite material; Tension (geology); Modulus; Strain (injury); Ultimate tensile strength; Strain energy release rate; Crystallography; Fracture mechanics; Chemistry; Computational chemistry; Physics; Optics","score_opus":0.10668163232603782,"score_gpt":0.3476001913590524,"score_spread":0.24091855903301457,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4281618614","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9673004,0.00024641538,0.024833325,0.00029917265,0.000020559863,0.000020893176,0.0002377595,0.00006692463,0.0069745784],"genre_scores_gemma":[0.996071,0.0001944451,0.0032467672,0.000013381903,0.0000045277193,0.000008920613,0.00006264855,0.000010620155,0.00038771617],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99997437,0.000004162901,0.0000012834547,0.0000048428205,0.000008679019,0.0000065542044],"domain_scores_gemma":[0.9999132,0.00003253557,0.000016712518,0.000012787856,0.000015959398,0.000008751169],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008955559,0.00025957244,0.00016332169,0.0002224944,0.00022914003,0.00032886758,0.00022909438,0.00038550128,0.0015227507],"category_scores_gemma":[0.00029743963,0.00014851085,0.00028175025,0.00019233164,0.00026579457,0.0005573236,0.00017485901,0.0003047315,0.00011340198],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000061100225,0.00011469706,0.012005823,0.00011480331,0.000053351545,0.00022943712,0.00010646357,0.89547086,0.07486311,0.010159058,0.00035106135,0.006470269],"study_design_scores_gemma":[0.000006672506,0.00001664842,0.0025767295,0.000004483957,0.0000050818467,0.000019207098,0.000022528131,0.9937557,0.0019942618,0.0012844121,0.0003090066,0.0000052068517],"about_ca_topic_score_codex":0.0061030667,"about_ca_topic_score_gemma":0.004238497,"teacher_disagreement_score":0.0061030667,"about_ca_system_score_codex":0.0002533056,"about_ca_system_score_gemma":0.0004305343,"threshold_uncertainty_score":0.012135088},"labels":[],"label_agreement":null},{"id":"W4281836580","doi":"10.1029/2022jb024250","title":"Subducting Indian Lithosphere Controls the Deep Carbon Emission in Lhasa Terrane, Southern Tibet","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Geology; Mantle (geology); Terrane; Mantle wedge; Subduction; Geochemistry; Asthenosphere; Continental crust; Lithosphere; Hotspot (geology); Earth science; Geophysics; Tectonics; Paleontology","score_opus":0.02615590142779006,"score_gpt":0.2782156755422261,"score_spread":0.25205977411443603,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4281836580","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995302,0.000036535337,0.0000283552,0.000010648341,7.7589397e-7,0.0000010628086,0.000068305126,0.00000339643,0.00032080943],"genre_scores_gemma":[0.99963176,0.000028057331,0.000021475693,0.000006381709,0.0000022155261,0.0000014861618,0.00013841367,0.0000019347854,0.00016815352],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995923,0.0000069581174,0.0000029603234,0.000011906553,0.0000057413254,0.000013260254],"domain_scores_gemma":[0.9999068,0.000013829544,0.000023912678,0.0000047418253,0.000018546061,0.000032046344],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010745475,0.00021767743,0.0001596211,0.0007963951,0.0004016757,0.00058399106,0.0001872392,0.00019020755,0.0011611626],"category_scores_gemma":[0.0001325706,0.0001276463,0.00014173548,0.0006947592,0.00033207834,0.00016487118,0.00028643102,0.000108024215,0.00014447406],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002930367,0.000040494502,0.86122996,0.000054065502,0.00011097351,0.0007043993,0.0009983549,0.0011710261,0.12880401,0.0002041376,0.00017092713,0.006218671],"study_design_scores_gemma":[0.0000045459915,0.000016739668,0.99838495,0.0000031948093,0.000010404172,0.000044122924,0.0003389143,0.00054312724,0.00048589037,0.000027303484,0.00013796893,0.0000029044886],"about_ca_topic_score_codex":0.024836611,"about_ca_topic_score_gemma":0.027049173,"teacher_disagreement_score":0.024836611,"about_ca_system_score_codex":0.0003668797,"about_ca_system_score_gemma":0.00022615798,"threshold_uncertainty_score":0.049384058},"labels":[],"label_agreement":null},{"id":"W4283158767","doi":"10.1029/2021jb023419","title":"Differentiating Fissure‐Fed Lava Flow Types and Facies Using RADAR and LiDAR: An Example From the 2014–2015 Holuhraun Lava Flow‐Field","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Lava; Geology; Facies; Lava field; Volcano; Radar; Lidar; Remote sensing; Petrology; Geomorphology; Seismology","score_opus":0.07079610893949512,"score_gpt":0.3260601836943155,"score_spread":0.2552640747548204,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4283158767","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970209,0.00011202826,0.0007226986,0.00007326108,0.000008120696,0.000019258357,0.00082772,0.000058071353,0.0011579284],"genre_scores_gemma":[0.9953087,0.00005379445,0.0029804148,0.000024429935,0.000012510047,0.000009812911,0.0013128185,0.0000104280325,0.00028716555],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99978167,0.000023674667,0.00001874214,0.00004789699,0.00007019156,0.000057807974],"domain_scores_gemma":[0.99937916,0.00013113533,0.000098683,0.000054145763,0.0002445474,0.00009232445],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00052670593,0.00018576237,0.00023047485,0.0024136892,0.00054842746,0.00043377848,0.00033132095,0.00037920105,0.00041751395],"category_scores_gemma":[0.0005485219,0.0000962934,0.00034795032,0.0013876805,0.00032684655,0.0003270192,0.0003943968,0.00026110566,0.0001325218],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002476559,0.00045505824,0.8849244,0.00011181733,0.00015070404,0.0018834459,0.0012595927,0.0071221716,0.022599488,0.00043678275,0.0030773517,0.07773153],"study_design_scores_gemma":[0.000008919304,0.000041037172,0.98507315,0.000015291713,0.000024513438,0.00020034559,0.0005906127,0.011080872,0.0015096035,0.000090667076,0.0013473092,0.0000178209],"about_ca_topic_score_codex":0.03634993,"about_ca_topic_score_gemma":0.0914867,"teacher_disagreement_score":0.03634993,"about_ca_system_score_codex":0.00052592484,"about_ca_system_score_gemma":0.00043993746,"threshold_uncertainty_score":0.07227671},"labels":[],"label_agreement":null},{"id":"W4283582315","doi":"10.1029/2021jb022621","title":"Aseismic Fault Slip During a Shallow Normal‐Faulting Seismic Swarm Constrained Using a Physically Informed Geodetic Inversion Method","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"University of Liverpool; Natural Environment Research Council; Sight Research UK","keywords":"Slip (aerodynamics); Seismology; Geology; Interferometric synthetic aperture radar; Geodetic datum; Slipping; Geodesy; Episodic tremor and slip; Tectonics; Geometry; Synthetic aperture radar; Subduction; Mathematics; Remote sensing; Engineering","score_opus":0.050034415162463056,"score_gpt":0.3408482736245999,"score_spread":0.29081385846213686,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4283582315","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8723887,0.00006265,0.1259017,0.00016578598,0.000015645452,0.000025358433,0.0001435159,0.00022307198,0.0010736218],"genre_scores_gemma":[0.9814285,0.000019677296,0.018053744,0.000017643055,0.000010619823,0.000015015979,0.00013278572,0.000013569211,0.00030845028],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999505,0.000012245917,0.0000035185328,0.00001510448,0.0000097943885,0.000008784374],"domain_scores_gemma":[0.9998696,0.0000441783,0.0000341585,0.000015559639,0.000023647322,0.0000129099535],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002076137,0.00032588787,0.00022667284,0.0002681651,0.00014807054,0.0003284067,0.00048302097,0.00043632754,0.00047756082],"category_scores_gemma":[0.00055290933,0.00024428777,0.0003047693,0.00019829119,0.00030637742,0.00025782935,0.00023982105,0.00034737826,0.00005724019],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007926587,0.00006206738,0.008013043,0.000026627064,0.00004467051,0.00011788917,0.0000618877,0.9602704,0.013973755,0.00097042974,0.00022954983,0.016150516],"study_design_scores_gemma":[0.0000042760116,0.0000040142027,0.000948548,8.1846673e-7,0.000001946005,0.0000035902838,0.0000035019411,0.99862564,0.00029964722,0.00007217126,0.00003363196,0.0000022781678],"about_ca_topic_score_codex":0.010072242,"about_ca_topic_score_gemma":0.010978889,"teacher_disagreement_score":0.010072242,"about_ca_system_score_codex":0.00026115746,"about_ca_system_score_gemma":0.0005705612,"threshold_uncertainty_score":0.02002722},"labels":[],"label_agreement":null},{"id":"W4283590977","doi":"10.1029/2021jb023322","title":"Possible Effects of Multiphase Methane Evolution During a Glacial Cycle on Underpressure Development in Sedimentary Basins: An Analysis With Application to the Northeast Michigan Basin","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Nuclear Waste Management Organization","keywords":"Methane; Geology; Sedimentary rock; Pore water pressure; Permeability (electromagnetism); Glacial period; Geochemistry; Petrology; Soil science; Geomorphology; Chemistry; Geotechnical engineering","score_opus":0.008324479272975483,"score_gpt":0.2783084886348062,"score_spread":0.2699840093618307,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4283590977","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996486,0.000009484661,0.00011946518,0.000016164648,6.779296e-7,0.0000032380603,0.000042926862,0.000011744664,0.00014770281],"genre_scores_gemma":[0.9996518,0.000014947065,0.00021041294,0.0000028049587,9.669237e-7,0.000003893252,0.000050161194,0.0000035257638,0.0000614572],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991345,0.00001942449,0.00000786804,0.000016445229,0.000020607138,0.000022129645],"domain_scores_gemma":[0.9996532,0.00017503377,0.000051801206,0.00002454638,0.000050412855,0.00004497598],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002472772,0.0003507287,0.00029919075,0.000696308,0.0006497462,0.00072714797,0.0005317884,0.00073820446,0.00073301134],"category_scores_gemma":[0.0010697498,0.00036838645,0.0006271468,0.00063257443,0.0005087044,0.00041614546,0.0004236868,0.0002784087,0.00005671147],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003663281,0.00027788783,0.54288983,0.00007007715,0.00019829618,0.0008326969,0.0002655025,0.41516545,0.031930774,0.0005174027,0.00019092123,0.0072948537],"study_design_scores_gemma":[0.000035346828,0.00014558595,0.28361446,0.0000065387117,0.00004866924,0.000060341532,0.0001843544,0.7113017,0.004257094,0.00011470605,0.00020631302,0.000024935334],"about_ca_topic_score_codex":0.10330645,"about_ca_topic_score_gemma":0.07273089,"teacher_disagreement_score":0.8966935,"about_ca_system_score_codex":0.0019049929,"about_ca_system_score_gemma":0.00084818905,"threshold_uncertainty_score":0.20541024},"labels":[],"label_agreement":null},{"id":"W4285094034","doi":"10.1029/2021jb023749","title":"Quantifying Interdependencies in Geyser Eruptions at the Upper Geyser Basin, Yellowstone National Park","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Species Distribution and Climate Change","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Structural basin; National park; Earth science; Seismology; Paleontology; Geography; Archaeology","score_opus":0.12060751100589438,"score_gpt":0.3897172482491577,"score_spread":0.2691097372432633,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4285094034","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992473,0.000021247906,0.00027491603,0.000020031539,7.6333777e-7,0.0000052774135,0.00024752415,0.000008435616,0.00017450878],"genre_scores_gemma":[0.9990631,0.00002059755,0.00042585583,0.000006355225,0.0000014718235,0.00000735394,0.0003734815,0.000002394902,0.00009944895],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999757,0.000048023598,0.00001811513,0.00010094446,0.00004351022,0.000032379936],"domain_scores_gemma":[0.99930024,0.00027081353,0.00016630851,0.000074733274,0.00009530124,0.0000926351],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00068135065,0.0001705409,0.00024334072,0.0007964176,0.00034305922,0.0005197649,0.00036615352,0.00027154345,0.0005842165],"category_scores_gemma":[0.0017634648,0.00014867961,0.00025082924,0.0008043637,0.00033785202,0.0005159995,0.00088883884,0.00025477918,0.00005483523],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000037154936,0.000034510453,0.9844109,0.000011596875,0.00007350689,0.00009278035,0.000321169,0.0081994645,0.0018870032,0.00009806346,0.00015607198,0.004677777],"study_design_scores_gemma":[0.0000037041616,0.000015113878,0.97907937,0.000004460238,0.000012876793,0.000018808092,0.00025494656,0.019987244,0.00026541512,0.00010744604,0.00024699618,0.0000037209759],"about_ca_topic_score_codex":0.0908458,"about_ca_topic_score_gemma":0.20826277,"teacher_disagreement_score":0.0908458,"about_ca_system_score_codex":0.0009661539,"about_ca_system_score_gemma":0.0005515195,"threshold_uncertainty_score":0.18063402},"labels":[],"label_agreement":null},{"id":"W4286299818","doi":"10.1029/2022jb024031","title":"Age and Rate of Accumulation of Metal‐Rich Hydrothermal Deposits on the Seafloor: The Lucky Strike Vent Field, Mid‐Atlantic Ridge","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs","keywords":"Hydrothermal circulation; Seafloor spreading; Mid-Atlantic Ridge; Geology; Ridge; Hydrothermal vent; Mid-ocean ridge; Geochemistry; Tectonics; Paleontology","score_opus":0.06400096893437199,"score_gpt":0.31501647168772484,"score_spread":0.2510155027533528,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4286299818","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991404,0.000059461785,0.00003817047,0.0000061247783,7.6518165e-7,0.0000011131746,0.00029166634,0.0000072652842,0.00045506508],"genre_scores_gemma":[0.99891925,0.00004347832,0.000059378814,0.000005088808,0.0000014281097,0.0000012904713,0.00042584143,0.0000027866954,0.00054144877],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994826,0.0000047860694,0.0000034503817,0.000019619649,0.000007806636,0.000016102123],"domain_scores_gemma":[0.9996649,0.000053277836,0.000106690146,0.000018644669,0.00008540985,0.000071122486],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013613704,0.00015615126,0.000110174944,0.0010737246,0.00015944724,0.0004093836,0.0001623542,0.00015676292,0.0011369847],"category_scores_gemma":[0.00032867573,0.00012494493,0.0001013658,0.0003751111,0.00021558035,0.00023409385,0.00021506136,0.00011144546,0.0003636133],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020433783,0.000011628209,0.9730502,0.0000126779305,0.000031190633,0.000104498606,0.00019727174,0.00015970509,0.020428775,0.00003206796,0.00013649426,0.005631141],"study_design_scores_gemma":[8.587143e-7,0.000013219181,0.9992824,8.4042847e-7,0.000002283735,0.000028318287,0.000035888665,0.00006760424,0.00046954514,0.000002836936,0.0000949013,0.0000012973436],"about_ca_topic_score_codex":0.023986101,"about_ca_topic_score_gemma":0.04212027,"teacher_disagreement_score":0.023986101,"about_ca_system_score_codex":0.00034665706,"about_ca_system_score_gemma":0.0001433275,"threshold_uncertainty_score":0.047692955},"labels":[],"label_agreement":null},{"id":"W4289523175","doi":"10.1029/2022jb024494","title":"The Effect of a Weak Asthenospheric Layer on Surface Kinematics, Subduction Dynamics and Slab Morphology in the Lower Mantle","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Agence Nationale de la Recherche","keywords":"Slab; Subduction; Geology; Mantle (geology); Kinematics; Slab window; Seismology; Geophysics; Petrology; Tectonics; Oceanic crust; Physics","score_opus":0.016023547870523305,"score_gpt":0.2896933028158653,"score_spread":0.273669754945342,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4289523175","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999542,0.00003405696,0.00016260846,0.000014347319,0.0000022018974,0.000001083368,0.000027768663,0.000009534488,0.00020651147],"genre_scores_gemma":[0.99985623,0.000012524934,0.00006790872,0.0000034078053,7.2559266e-7,6.198066e-7,0.000015073442,0.000001625056,0.000041884494],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999441,0.000010792495,0.0000050779545,0.00001007175,0.000008761618,0.000021123993],"domain_scores_gemma":[0.99980193,0.00006265197,0.000048886235,0.000020948271,0.000017497445,0.00004805517],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015428539,0.0003906169,0.0002164491,0.00027846073,0.0002721917,0.0007061414,0.00032106077,0.00030629386,0.0011081785],"category_scores_gemma":[0.0006158427,0.00020825071,0.0003611565,0.00014771812,0.0006096689,0.0003290981,0.00054499134,0.00032356355,0.00010557414],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015651028,0.00023363427,0.24345274,0.00017485954,0.0003580457,0.00052565354,0.0001564735,0.25393552,0.48783535,0.0016581543,0.00021886143,0.00988554],"study_design_scores_gemma":[0.00022762647,0.0010814866,0.4794949,0.000039570226,0.00041730906,0.0001309165,0.00036445475,0.41976744,0.096818574,0.00089619315,0.0007133807,0.000048180413],"about_ca_topic_score_codex":0.0070443335,"about_ca_topic_score_gemma":0.0040558265,"teacher_disagreement_score":0.0070443335,"about_ca_system_score_codex":0.00041902094,"about_ca_system_score_gemma":0.0002530181,"threshold_uncertainty_score":0.014006674},"labels":[],"label_agreement":null},{"id":"W4290099076","doi":"10.1029/2022jb024584","title":"Application of Machine Learning to Characterizing Magma Fertility in Porphyry Cu Deposits","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Lakehead University","funders":"National Natural Science Foundation of China","keywords":"Zircon; Geology; Subduction; Magma; Geochemistry; Porphyry copper deposit; Igneous rock; Crust; Random forest; A priori and a posteriori; Machine learning; Seismology; Computer science; Tectonics; Volcano; Fluid inclusions; Hydrothermal circulation","score_opus":0.029354718962227428,"score_gpt":0.31596747417308224,"score_spread":0.28661275521085483,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4290099076","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.964314,0.00018484311,0.034640763,0.00006112401,0.000007227789,0.000025579957,0.00011950233,0.00023039928,0.00041661953],"genre_scores_gemma":[0.99440104,0.000025427677,0.0053753597,0.0000061760916,0.0000021510828,0.000007177385,0.00007559449,0.000003823867,0.000103406455],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998016,0.000068007015,0.0000120122995,0.00005679067,0.000033109092,0.000028458488],"domain_scores_gemma":[0.99930406,0.00036547714,0.000093982686,0.000071335344,0.00013517705,0.000029941999],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009868658,0.0006703051,0.00033997121,0.0009422959,0.0002715274,0.0004719806,0.00051722117,0.00053922256,0.0002337076],"category_scores_gemma":[0.0018737476,0.00017809376,0.00038721377,0.0005666275,0.0003138255,0.00037389112,0.00030172698,0.00037432267,0.00009023891],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000078500634,0.00008254948,0.044347327,0.000029107245,0.000072296534,0.000102216814,0.00006151763,0.907018,0.0060915407,0.00015781919,0.00016346839,0.04179571],"study_design_scores_gemma":[0.000002070726,0.0000153226,0.0047841794,0.0000019313347,0.0000033227411,0.00001025312,0.000012640705,0.9937994,0.0012068576,0.00012082378,0.000039639097,0.0000035359499],"about_ca_topic_score_codex":0.022312239,"about_ca_topic_score_gemma":0.018172234,"teacher_disagreement_score":0.022312239,"about_ca_system_score_codex":0.0008617592,"about_ca_system_score_gemma":0.0005889912,"threshold_uncertainty_score":0.04436469},"labels":[],"label_agreement":null},{"id":"W4292712481","doi":"10.1029/2022jb024744","title":"Spatiotemporal Variations in Earthquake Triggering Mechanisms During Multistage Hydraulic Fracturing in Western Canada","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seismology; Induced seismicity; Hydraulic fracturing; Magnitude (astronomy); Pore water pressure; Fault (geology); Fracture (geology); Geotechnical engineering","score_opus":0.02855768288526143,"score_gpt":0.28538316221635296,"score_spread":0.2568254793310915,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4292712481","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996591,0.00011542456,0.00018930809,0.000042932217,0.0000023674456,0.000010866731,0.0019104722,0.00001779592,0.0011199642],"genre_scores_gemma":[0.99772924,0.00009578408,0.00024413296,0.000012373018,0.0000014873535,0.0000051288375,0.0011119773,0.0000037995828,0.00079600036],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99978274,0.000007562644,0.000008188008,0.00004629042,0.00006982663,0.000085377236],"domain_scores_gemma":[0.99917644,0.000047052672,0.00011976858,0.000023878676,0.00047311015,0.00015962118],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000164969,0.00029074016,0.00022295969,0.0017414446,0.0010029351,0.00091219123,0.0006500587,0.00026220182,0.001081925],"category_scores_gemma":[0.0006539209,0.0001886535,0.00015121083,0.0030118034,0.0005815928,0.00018942477,0.00058006076,0.00022595085,0.00015843802],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014397906,0.00003200995,0.9662788,0.000048409653,0.0000686632,0.00037716003,0.0019637302,0.0016345858,0.00876813,0.00022166736,0.0010798379,0.019383157],"study_design_scores_gemma":[0.0000021758497,0.0000057802513,0.99732035,0.000008037967,0.000009212463,0.00002682943,0.0010223257,0.0007633517,0.00027100331,0.000014457471,0.00054804166,0.000008440484],"about_ca_topic_score_codex":0.98971295,"about_ca_topic_score_gemma":0.9958377,"teacher_disagreement_score":0.010287046,"about_ca_system_score_codex":0.00914831,"about_ca_system_score_gemma":0.009144365,"threshold_uncertainty_score":0.06637597},"labels":[],"label_agreement":null},{"id":"W4293067972","doi":"10.1029/2021jb023722","title":"Evaluating the Tsunamigenic Potential of Buried Versus Trench‐Breaching Megathrust Slip","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Seafloor spreading; Trench; Subduction; Slip (aerodynamics); Seismology; Episodic tremor and slip; Tsunami earthquake; Thickening; Deformation (meteorology); Tectonics; Geophysics","score_opus":0.12211788151624407,"score_gpt":0.39711334012206206,"score_spread":0.274995458605818,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4293067972","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99904853,0.0000431356,0.0004415581,0.000009147272,0.0000017926312,0.00000355323,0.00005327607,0.000010137803,0.00038890092],"genre_scores_gemma":[0.9996966,0.000016317043,0.00017030435,0.0000018176843,7.795383e-7,0.0000015878697,0.00003797819,0.0000014746977,0.000073091236],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999013,0.000020326237,0.000007833953,0.000018636367,0.000019996609,0.00003180952],"domain_scores_gemma":[0.999278,0.00038667102,0.00012683553,0.00003882268,0.00007312183,0.00009648023],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039753775,0.00045044158,0.00031965156,0.00062125985,0.0001824734,0.000573148,0.00033196848,0.000501122,0.001052351],"category_scores_gemma":[0.0013174572,0.00021159263,0.00036219053,0.0004022664,0.00033515805,0.00047688483,0.0003985013,0.00024047773,0.00010792475],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000678325,0.00017560057,0.13456103,0.00007946075,0.00013205515,0.00039540793,0.00006400495,0.83849454,0.01667727,0.00061976403,0.00011585456,0.008006691],"study_design_scores_gemma":[0.000024068531,0.000669911,0.07460892,0.000013717865,0.000050183942,0.00007058682,0.00019920175,0.9179266,0.0059402664,0.0003556688,0.00011779587,0.000023174489],"about_ca_topic_score_codex":0.005021014,"about_ca_topic_score_gemma":0.0052011157,"teacher_disagreement_score":0.005021014,"about_ca_system_score_codex":0.0004944291,"about_ca_system_score_gemma":0.0002146242,"threshold_uncertainty_score":0.00998354},"labels":[],"label_agreement":null},{"id":"W4295037292","doi":"10.1029/2022jb024354","title":"Limited Earthquake Interaction During a Geothermal Hydraulic Stimulation in Helsinki, Finland","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Hotchkiss Brain Institute; University of Calgary","funders":"Helmholtz Association","keywords":"Induced seismicity; Geophone; Geothermal gradient; Seismology; Geology; Hydraulic fracturing; Magnitude (astronomy); Borehole; Rock mass classification; Geophysics; Geotechnical engineering; Physics","score_opus":0.045155125991264485,"score_gpt":0.31703675698758316,"score_spread":0.2718816309963187,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4295037292","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996798,0.000006083319,0.00006484549,0.000003873444,6.988365e-7,0.0000024334704,0.000045719065,0.0000037327252,0.00019281],"genre_scores_gemma":[0.9998399,0.0000049057744,0.000024651355,0.0000016608852,0.0000012418867,0.0000023912482,0.00006289118,4.4282098e-7,0.00006197191],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988914,0.000016179072,0.0000074093673,0.000023348042,0.000032211727,0.000031755546],"domain_scores_gemma":[0.9996871,0.000086912136,0.000094808354,0.00002013787,0.000041492352,0.00006955073],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015879754,0.00015053453,0.00018514275,0.00040175268,0.00018972174,0.00022657777,0.00019192658,0.00028660777,0.0008227097],"category_scores_gemma":[0.0004906434,0.00010202932,0.00011338521,0.00039611047,0.0002828376,0.00017377813,0.0003761739,0.00012309184,0.000091283015],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011372279,0.00036259956,0.87270457,0.000115791976,0.00016786881,0.0026916703,0.0015488437,0.013445518,0.09123567,0.00018053183,0.00041729544,0.015992489],"study_design_scores_gemma":[0.0000107419255,0.00024134059,0.9919384,0.0000043635373,0.000021317608,0.00010471531,0.00047909326,0.003908754,0.003039041,0.0000273771,0.00021457562,0.000010134446],"about_ca_topic_score_codex":0.0037671993,"about_ca_topic_score_gemma":0.0075064483,"teacher_disagreement_score":0.0037671993,"about_ca_system_score_codex":0.00038985204,"about_ca_system_score_gemma":0.00026811348,"threshold_uncertainty_score":0.0074905157},"labels":[],"label_agreement":null},{"id":"W4296018147","doi":"10.1029/2022jb023987","title":"Structure and Evolution of Northern Juan de Fuca Crust and Uppermost Mantle Over the Last 8 Ma From an Active‐Source Seismic Tomography Study","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Science Foundation","keywords":"Geology; Crust; Subduction; Mantle (geology); Seismology; Oceanic crust; Transect; Continental crust; Petrology; Geophysics; Tectonics; Oceanography","score_opus":0.014139940056248674,"score_gpt":0.28098700535909926,"score_spread":0.2668470653028506,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4296018147","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981371,0.00015504271,0.000077336714,0.000029140027,0.000001905024,0.0000032625278,0.00026687543,0.000013460809,0.0013158921],"genre_scores_gemma":[0.9990189,0.00010207279,0.00016757657,0.0000057509455,0.0000030737183,0.00000386899,0.0003876371,0.0000043915006,0.000306639],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999168,0.0000062413724,0.000005670009,0.00003155169,0.00002039572,0.00001926547],"domain_scores_gemma":[0.99983835,0.000014634437,0.000050825456,0.00001774234,0.00005009965,0.000028371544],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026639987,0.00039376304,0.00020625818,0.0012297245,0.00047690532,0.00069326215,0.00026474168,0.0003128093,0.0009067264],"category_scores_gemma":[0.00054082775,0.00025175407,0.00034870615,0.0010497931,0.00034609158,0.00023978997,0.0005977087,0.00019011543,0.0001527475],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012601823,0.000031304047,0.9553177,0.00006420742,0.00023573366,0.0003441679,0.001404988,0.0026806854,0.024024012,0.00018689373,0.00018106986,0.01540331],"study_design_scores_gemma":[0.0000028841437,0.000009872152,0.99817014,0.000008261356,0.000019977035,0.00006573077,0.00019444224,0.0005772636,0.00033841576,0.000017873568,0.00059066335,0.000004477798],"about_ca_topic_score_codex":0.10913245,"about_ca_topic_score_gemma":0.16975477,"teacher_disagreement_score":0.10913245,"about_ca_system_score_codex":0.0011364969,"about_ca_system_score_gemma":0.0005881792,"threshold_uncertainty_score":0.21699446},"labels":[],"label_agreement":null},{"id":"W4297143959","doi":"10.1029/2021jb023444","title":"Insights on Multistage Rock Avalanche Behavior From Runout Modeling Constrained by Seismic Inversions","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Northern British Columbia; BGC Engineering (Canada); University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Landslide; Seismology; Rheology; Inversion (geology); Calibration; Geotechnical engineering","score_opus":0.02725836954066482,"score_gpt":0.29869273281109104,"score_spread":0.27143436327042625,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4297143959","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.91144794,0.000056621695,0.086375594,0.0000735013,0.000004561669,0.000027429176,0.00014246561,0.00025010674,0.0016218056],"genre_scores_gemma":[0.99466586,0.0000328338,0.0050095706,0.000004483491,0.0000028091963,0.000010548807,0.00006721438,0.000024146046,0.00018245445],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992335,0.000024114539,0.0000053028466,0.0000195117,0.000013609339,0.000014211807],"domain_scores_gemma":[0.9995065,0.00030420275,0.000078224424,0.000039908802,0.00003955664,0.00003158106],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005740375,0.0005523436,0.00034428886,0.00043711727,0.00017970883,0.000664656,0.0005570724,0.00048265414,0.00075958227],"category_scores_gemma":[0.0017981697,0.0003476108,0.00042349013,0.00025894164,0.0004435276,0.0005250155,0.0003980313,0.00048337263,0.00006128665],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020463267,0.000021954278,0.004951225,0.000011323847,0.000017848139,0.00006822351,0.000042159143,0.9887925,0.0029616875,0.0006984608,0.000033751865,0.0023803636],"study_design_scores_gemma":[0.0000015595256,0.000003415435,0.0007154783,0.0000010570519,0.0000014262113,0.000003010422,0.0000047496733,0.998988,0.0001292933,0.00013263599,0.000017392713,0.0000019675542],"about_ca_topic_score_codex":0.010554204,"about_ca_topic_score_gemma":0.010070849,"teacher_disagreement_score":0.010554204,"about_ca_system_score_codex":0.00040632958,"about_ca_system_score_gemma":0.0006515178,"threshold_uncertainty_score":0.020985544},"labels":[],"label_agreement":null},{"id":"W4297359859","doi":"10.1029/2022jb024130","title":"The Structure and Dynamics of the Uppermost Mantle of Southwestern Canada From a Joint Analysis of Geophysical Observations","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Asthenosphere; Mantle (geology); Lithosphere; Geology; Craton; Olivine; Geophysics; Low-velocity zone; Petrology; Geochemistry; Seismology; Tectonics","score_opus":0.025633101016576343,"score_gpt":0.2570106688271588,"score_spread":0.23137756781058244,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4297359859","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962469,0.00028420807,0.00013937498,0.00007121382,0.0000028241514,0.0000076011906,0.0022809152,0.000033587705,0.0009332975],"genre_scores_gemma":[0.994926,0.00019697653,0.00052249234,0.000021912761,0.00000320322,0.0000063263738,0.003513503,0.0000073711344,0.0008022261],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998041,0.0000059576882,0.000009123329,0.000048052527,0.00006358868,0.000069091446],"domain_scores_gemma":[0.999511,0.000020898442,0.00006194,0.00002108108,0.00029004336,0.000095088995],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019265484,0.00044020684,0.0002728267,0.0017961747,0.0013179893,0.00093463843,0.0004732052,0.00027041574,0.0011376645],"category_scores_gemma":[0.00055508164,0.00020208146,0.00044507816,0.0031824412,0.00031363947,0.00018246505,0.000655757,0.0002132522,0.0001507868],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000109657274,0.000024622785,0.9597373,0.000046982226,0.00020565328,0.00020280851,0.0005743828,0.004504695,0.008962134,0.000244426,0.0016308607,0.023756476],"study_design_scores_gemma":[0.0000051817347,0.0000036356707,0.99430424,0.000010529938,0.000033995435,0.000025665162,0.00027797342,0.0034296834,0.00046852557,0.000023918092,0.0014073218,0.000009386551],"about_ca_topic_score_codex":0.9886874,"about_ca_topic_score_gemma":0.99271154,"teacher_disagreement_score":0.011312604,"about_ca_system_score_codex":0.010425887,"about_ca_system_score_gemma":0.010829221,"threshold_uncertainty_score":0.07564539},"labels":[],"label_agreement":null},{"id":"W4297973559","doi":"10.1029/2022jb024471","title":"Finding Simplicity in the Complexity of Postseismic Coastal Uplift and Subsidence Following Great Subduction Earthquakes","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; McGill University; University of Victoria","funders":"","keywords":"Geology; Subduction; Seismology; Slip (aerodynamics); Forearc; Subsidence; Lithosphere; Trench; Tectonics; Geomorphology","score_opus":0.1008226732484277,"score_gpt":0.3390219616011674,"score_spread":0.23819928835273968,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4297973559","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99556136,0.000043189542,0.0033097507,0.00006738733,0.000004806427,0.0000061326873,0.000100965764,0.00002794154,0.00087844604],"genre_scores_gemma":[0.9995746,0.0000143338375,0.00024785282,0.0000043723408,0.0000015170558,0.0000022103259,0.000039545,0.0000035982016,0.00011184585],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999229,0.000016116417,0.000007696675,0.000027143764,0.000009493201,0.000016625341],"domain_scores_gemma":[0.9997931,0.00005698322,0.0000661235,0.000039549115,0.000020868367,0.000023381761],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019954164,0.0002126934,0.00016978708,0.00026501063,0.00015593877,0.0005324508,0.0003231215,0.00047710835,0.0006986234],"category_scores_gemma":[0.00078183605,0.00018282606,0.00038105788,0.00020563023,0.0004356943,0.00049868063,0.00038902953,0.00033381776,0.00007564441],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001303846,0.00014723817,0.19991481,0.00004789898,0.00015029976,0.00035115422,0.00028395804,0.7647845,0.019058451,0.0048306785,0.00039633358,0.009904268],"study_design_scores_gemma":[0.000012269,0.00005259766,0.11976123,0.000006346628,0.000018638593,0.000036985064,0.00007570077,0.877361,0.0011884993,0.0011172107,0.00035685935,0.000012639099],"about_ca_topic_score_codex":0.008766362,"about_ca_topic_score_gemma":0.005610784,"teacher_disagreement_score":0.008766362,"about_ca_system_score_codex":0.000384215,"about_ca_system_score_gemma":0.0002542439,"threshold_uncertainty_score":0.017430663},"labels":[],"label_agreement":null},{"id":"W4297983960","doi":"10.1029/2022jb025126","title":"Long‐Term Fluid Injection Can Expedite Fault Reactivation and Development: Riedel Shear Structures Illuminated by Induced Earthquakes in Alberta, Canada","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geoscience BC; University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Seismology; Induced seismicity; Shear (geology); Slip (aerodynamics); Lineament; RSS; Shear stress; Strike-slip tectonics; Active fault; Outcrop; Fault (geology); Tectonics; Petrology; Geomorphology; Engineering","score_opus":0.027194059656748735,"score_gpt":0.2772226014817455,"score_spread":0.25002854182499673,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4297983960","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99702877,0.00014632789,0.0001091021,0.00010628608,0.0000028810796,0.000010547641,0.00077874475,0.000013265649,0.0018040757],"genre_scores_gemma":[0.99796695,0.00012242231,0.00016770563,0.000016853011,0.0000016374746,0.0000029636362,0.0004805422,0.0000034980396,0.0012373459],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998301,0.000008821091,0.0000073282026,0.000026753607,0.00004964105,0.00007743466],"domain_scores_gemma":[0.99968886,0.000023377539,0.00004724636,0.000010064551,0.00014677062,0.00008376155],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001429782,0.0002453522,0.00020712888,0.0013389201,0.0013467554,0.0009137513,0.0006368861,0.00040367086,0.0016115276],"category_scores_gemma":[0.00040859295,0.0001730613,0.00020871825,0.0022837992,0.00064957066,0.00018646261,0.00051152625,0.00025592686,0.00014327858],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020970732,0.00009352914,0.96077895,0.00008323011,0.00009857979,0.0014808483,0.0039744466,0.0037945004,0.005706776,0.0006801279,0.0019086432,0.021190679],"study_design_scores_gemma":[0.000005757292,0.0000126916575,0.9932766,0.000013673549,0.00001696475,0.000046974168,0.003398348,0.0017480932,0.00018688412,0.000041928615,0.0012389731,0.000013171875],"about_ca_topic_score_codex":0.9907755,"about_ca_topic_score_gemma":0.99708694,"teacher_disagreement_score":0.013513257,"about_ca_system_score_codex":0.013513257,"about_ca_system_score_gemma":0.01316511,"threshold_uncertainty_score":0.098046005},"labels":[],"label_agreement":null},{"id":"W4300817537","doi":"10.1029/2022jb024881","title":"Analysis of the Hydrogeological Conditions Affecting Fault Response to Nearby Hydraulic Fracturing","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"University Research Board, American University of Beirut","keywords":"Induced seismicity; Hydrogeology; Hydraulic fracturing; Geology; Fault (geology); Pore water pressure; Petrology; Seismology; Microseism; Geotechnical engineering","score_opus":0.04006466938936335,"score_gpt":0.3358536811700587,"score_spread":0.29578901178069533,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4300817537","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997017,0.000008106046,0.000098955206,0.0000030806748,5.385491e-7,0.0000020326218,0.00004520379,0.0000040690825,0.00013626002],"genre_scores_gemma":[0.9998889,0.000004216551,0.000027799715,7.040471e-7,3.121724e-7,5.525138e-7,0.000032995853,5.153337e-7,0.000043942793],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992156,0.000008618048,0.000004934517,0.000014744986,0.000022153643,0.000027995162],"domain_scores_gemma":[0.99964714,0.0000613453,0.00011805968,0.000017872604,0.00009302258,0.000062468964],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000120876604,0.00014896896,0.00018077988,0.0007648658,0.00025545977,0.00043505518,0.00019171077,0.00022945442,0.0006782212],"category_scores_gemma":[0.00059559435,0.00007456462,0.00013120909,0.0005003509,0.00035174968,0.00015104741,0.0001774999,0.00011867736,0.000093494775],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030748866,0.00007499188,0.8872616,0.000042414846,0.000058881058,0.00071523373,0.0003881931,0.011376394,0.092177995,0.00010454485,0.00010286947,0.0073892777],"study_design_scores_gemma":[0.000001451112,0.00003692578,0.99277425,0.0000012959147,0.000006632372,0.000034628276,0.00030516114,0.0046360716,0.0021190098,0.000016916903,0.000063007436,0.0000047050025],"about_ca_topic_score_codex":0.036541328,"about_ca_topic_score_gemma":0.04396227,"teacher_disagreement_score":0.036541328,"about_ca_system_score_codex":0.0005667647,"about_ca_system_score_gemma":0.00032916118,"threshold_uncertainty_score":0.07265729},"labels":[],"label_agreement":null},{"id":"W4307291243","doi":"10.1029/2022jb024401","title":"Spatiotemporal Graph Convolutional Networks for Earthquake Source Characterization","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismology and Earthquake Studies","field":"Computer Science","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Los Alamos National Laboratory; National Institute of General Medical Sciences; Natural Sciences and Engineering Research Council of Canada; National Institutes of Health","keywords":"Computer science; Graph; Earthquake location; Artificial neural network; Convolutional neural network; Seismology; Earthquake simulation; Warning system; Earthquake prediction; Data mining; Artificial intelligence; Geology; Theoretical computer science; Induced seismicity","score_opus":0.041404116510293576,"score_gpt":0.3191178947058325,"score_spread":0.27771377819553894,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4307291243","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.10337439,0.0015111316,0.8846461,0.0008619013,0.00011465016,0.000048094702,0.0032511083,0.0028072451,0.0033854041],"genre_scores_gemma":[0.88272166,0.0010929838,0.10822816,0.00015895473,0.0000677939,0.000050772,0.004126788,0.00011440075,0.003438544],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998648,0.000021900461,0.000009400642,0.0000505529,0.00003106251,0.000022171407],"domain_scores_gemma":[0.99958616,0.00014641485,0.00008500333,0.00006857414,0.000093438066,0.000020450783],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002654818,0.00065284077,0.00030136705,0.0010279396,0.0002147632,0.0004375577,0.00071627065,0.00044874614,0.0012569394],"category_scores_gemma":[0.0018229228,0.00027861766,0.00047092407,0.0013961066,0.00028803662,0.0011018293,0.00042662228,0.00082614075,0.00029092454],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011039,0.000053645374,0.005904141,0.00010096624,0.0000951732,0.0001004984,0.000048010694,0.8321289,0.005128761,0.013473217,0.0044822004,0.13837413],"study_design_scores_gemma":[0.0000015005722,0.000005097085,0.0007829701,0.0000032661405,0.0000076034603,0.000008974262,0.0000043952855,0.99314404,0.000676164,0.0048207105,0.000541915,0.0000033805727],"about_ca_topic_score_codex":0.029204015,"about_ca_topic_score_gemma":0.04062197,"teacher_disagreement_score":0.029204015,"about_ca_system_score_codex":0.0011599372,"about_ca_system_score_gemma":0.00070021016,"threshold_uncertainty_score":0.058068037},"labels":[],"label_agreement":null},{"id":"W4307988587","doi":"10.1029/2022jb024004","title":"Effect of Ambient Humidity on the Elasticity and Deformation of Unweathered Granite","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Rock Mechanics and Modeling","field":"Engineering","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"China Scholarship Council","keywords":"Humidity; Relative humidity; Modulus; Poisson's ratio; Materials science; Composite material; Young's modulus; Moisture; Ambient pressure; Water content; Stress (linguistics); Adsorption; Elastic modulus; Mineralogy; Chemistry; Geology; Thermodynamics; Geotechnical engineering; Poisson distribution; Mathematics; Physics","score_opus":0.02650490872764063,"score_gpt":0.29839961936657033,"score_spread":0.2718947106389297,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4307988587","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99956316,0.000033545628,0.00014552962,0.0000031622378,0.000001748937,0.0000020639138,0.00007957424,0.000009590338,0.00016162997],"genre_scores_gemma":[0.99963176,0.000019008618,0.00009381897,0.0000027217075,5.109432e-7,0.0000020790185,0.00007521295,0.0000044732874,0.00017057855],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99986625,0.000009374012,0.00000855626,0.00003255887,0.000055200682,0.0000279804],"domain_scores_gemma":[0.99986875,0.000027764392,0.0000331158,0.000016365471,0.000031112086,0.000022825388],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012436142,0.00023919284,0.00019911249,0.0002371889,0.00016589684,0.000259669,0.00021502691,0.00018900658,0.0010483979],"category_scores_gemma":[0.00021810144,0.00013490797,0.00015384248,0.00021112387,0.0002513521,0.00013849793,0.0002244885,0.00019041677,0.00014391597],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022827704,0.000026273961,0.009567403,0.000028304054,0.000014583899,0.00011902924,0.000055557615,0.0010957104,0.9865003,0.000018039706,0.000020645752,0.00232585],"study_design_scores_gemma":[0.000011668294,0.0004266497,0.3032814,0.0000057619086,0.000022366565,0.00017969494,0.0002720644,0.0059769275,0.6887772,0.00004191608,0.0009789477,0.00002546352],"about_ca_topic_score_codex":0.0027565262,"about_ca_topic_score_gemma":0.0049049566,"teacher_disagreement_score":0.0027565262,"about_ca_system_score_codex":0.00019171316,"about_ca_system_score_gemma":0.00010454338,"threshold_uncertainty_score":0.0054810047},"labels":[],"label_agreement":null},{"id":"W4309334838","doi":"10.1029/2022jb024983","title":"Micromechanics and Strain Localization in Sand in the Ductile Regime","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Rock Mechanics and Modeling","field":"Engineering","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Defense Threat Reduction Agency; National Science Foundation","keywords":"Micromechanics; Breakage; Overburden pressure; Geology; Cataclastic rock; Materials science; Shear band; Brittleness; Grain size; Strain hardening exponent; Geotechnical engineering; Shear (geology); Composite material; Fault (geology)","score_opus":0.031906053746657496,"score_gpt":0.30202561699440744,"score_spread":0.27011956324774994,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4309334838","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992662,0.000043440734,0.0002813788,0.0000070663236,8.2073683e-7,0.00000418953,0.000082121216,0.000016240916,0.00029847058],"genre_scores_gemma":[0.9996044,0.000032601787,0.00014995794,0.0000025694528,4.9660423e-7,0.0000033734325,0.000042247066,0.0000021875817,0.00016217752],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998628,0.000008294312,0.0000121890935,0.000028486244,0.00004647993,0.00004171515],"domain_scores_gemma":[0.99974006,0.000038153114,0.0000877543,0.00003600674,0.000054303255,0.000043727912],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000118021446,0.00025367827,0.00017475466,0.00058951124,0.0003815166,0.00045244975,0.0002969874,0.00020630837,0.0014839973],"category_scores_gemma":[0.00022075091,0.00030541065,0.00012160437,0.00037132826,0.00088545727,0.00027711794,0.00037210595,0.00030504807,0.00011818215],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016772527,0.000023064942,0.015605487,0.000056914014,0.000018016523,0.00024165433,0.0002725349,0.0008074153,0.980271,0.00010354187,0.00003326027,0.0023994683],"study_design_scores_gemma":[0.000009398249,0.000282489,0.4837763,0.000009060188,0.000030003635,0.00031150592,0.0006349904,0.006593342,0.50765973,0.00008459029,0.0005851988,0.000023373497],"about_ca_topic_score_codex":0.014539822,"about_ca_topic_score_gemma":0.022461832,"teacher_disagreement_score":0.014539822,"about_ca_system_score_codex":0.0005629427,"about_ca_system_score_gemma":0.0003493873,"threshold_uncertainty_score":0.028910339},"labels":[],"label_agreement":null},{"id":"W4309624730","doi":"10.1029/2022jb024748","title":"Crustal Seismic Anisotropy Along the Continental Margin in Western Canada From Receiver Function Analysis","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; University of Calgary; University of Ottawa","funders":"","keywords":"Geology; Terrane; Seismology; Receiver function; Subduction; North American Plate; Tectonics; Crust; Lithosphere; Plate tectonics; Continental margin; Oceanic crust; Seismic hazard; Convergent boundary; Geophysics","score_opus":0.024006005920878027,"score_gpt":0.26983054460417544,"score_spread":0.2458245386832974,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4309624730","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9952813,0.00019141615,0.00029859104,0.00004308439,0.0000032886478,0.000006452876,0.0019566321,0.000037863025,0.0021813007],"genre_scores_gemma":[0.9968265,0.0001351826,0.00037021493,0.000009232383,0.0000016446363,0.0000025849763,0.0015657981,0.000008245617,0.0010806212],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998721,0.000004890969,0.0000047337853,0.000019920824,0.000050443126,0.00004785986],"domain_scores_gemma":[0.99957126,0.000021849479,0.000033520926,0.000012584081,0.0003064091,0.00005446559],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013877024,0.00043236124,0.00019832862,0.0016069838,0.00089893874,0.0008343752,0.00036111622,0.00017154013,0.0015723918],"category_scores_gemma":[0.0004452282,0.00017613209,0.00016193476,0.0028428556,0.00024794295,0.00014279112,0.00033659048,0.00019322716,0.00030857595],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016714212,0.000041319316,0.92643136,0.000050097224,0.00009098962,0.00046132933,0.0011668373,0.0060148444,0.017492557,0.00034634813,0.0022686669,0.045468617],"study_design_scores_gemma":[0.000004083777,0.0000051829984,0.9927946,0.000015297795,0.00002093339,0.00004369006,0.0006622821,0.004410181,0.00073506526,0.000029668025,0.0012687562,0.000010300666],"about_ca_topic_score_codex":0.98823535,"about_ca_topic_score_gemma":0.9935894,"teacher_disagreement_score":0.011764646,"about_ca_system_score_codex":0.0058599585,"about_ca_system_score_gemma":0.0073255757,"threshold_uncertainty_score":0.042517185},"labels":[],"label_agreement":null},{"id":"W4309761239","doi":"10.1029/2022jb023989","title":"Using Seafloor Geodesy to Detect Vertical Deformation at the Hikurangi Subduction Zone: Insights From Self‐Calibrating Pressure Sensors and Ocean General Circulation Models","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Directorate for Geosciences; Ministry for Business Innovation and Employment; Ministry of Education, Culture, Sports, Science and Technology","keywords":"Seafloor spreading; Geology; Subduction; Submarine pipeline; Seismology; Slip (aerodynamics); Trench; Geodesy; Tectonics; Oceanography","score_opus":0.04956741121461599,"score_gpt":0.2916262080576809,"score_spread":0.24205879684306492,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4309761239","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974873,0.00005574054,0.0019058656,0.00004433538,0.000005062074,0.0000040739387,0.0001060421,0.0000220044,0.00036939897],"genre_scores_gemma":[0.9985228,0.00004296403,0.0012122787,0.0000066953903,0.000002317341,0.0000018182392,0.00011067404,0.0000042384404,0.000096346484],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991226,0.000017667464,0.0000062396357,0.000030679163,0.000016106873,0.00001710072],"domain_scores_gemma":[0.99982315,0.00004630183,0.00004564659,0.000021484066,0.000041946907,0.000021535041],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003281538,0.00037259722,0.00018011782,0.0005417562,0.00016936909,0.00058774464,0.00023634911,0.0002660004,0.0003888662],"category_scores_gemma":[0.0009330768,0.00019778495,0.0003207065,0.0005279158,0.0002588481,0.00052338344,0.00033699023,0.00021817423,0.000092636954],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009918576,0.00007108016,0.914751,0.000036590187,0.00013439723,0.00028009666,0.00026149442,0.038851902,0.019665329,0.00030146772,0.00024109945,0.025306422],"study_design_scores_gemma":[0.000009137557,0.00004325076,0.7967189,0.000010900093,0.00003618754,0.000043284264,0.00019600466,0.20115736,0.001390422,0.0001235309,0.00025154848,0.000019385725],"about_ca_topic_score_codex":0.037550386,"about_ca_topic_score_gemma":0.048754662,"teacher_disagreement_score":0.037550386,"about_ca_system_score_codex":0.00031131046,"about_ca_system_score_gemma":0.00032317144,"threshold_uncertainty_score":0.07466364},"labels":[],"label_agreement":null},{"id":"W4310027127","doi":"10.1029/2022jb024719","title":"Monitoring CO<sub>2</sub> Injection at the CaMI Field Research Station Using Microseismic Noise Sources","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Carbon Management Canada; University of Calgary; University of Alberta","funders":"Canada First Research Excellence Fund; Natural Science Foundation of Chongqing; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Geophone; Microseism; Noise (video); Ambient noise level; Seismology; Passive seismic; Geology; Environmental science; Seismic noise; Environmental noise; Computer science; Geomorphology","score_opus":0.06415651111780153,"score_gpt":0.3575061738604764,"score_spread":0.2933496627426749,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4310027127","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954396,0.000047068155,0.001580331,0.000052557218,0.000006222511,0.0000162376,0.0006688046,0.00007825127,0.0021109951],"genre_scores_gemma":[0.9969965,0.00003871188,0.0013208893,0.000013879205,0.0000059557246,0.000009364605,0.00046164522,0.000007390949,0.0011457435],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998894,0.000005705687,0.0000026414236,0.000021614243,0.00006209827,0.000018611028],"domain_scores_gemma":[0.99979407,0.000018730829,0.000050057795,0.0000064095607,0.000105316976,0.000025386229],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008526158,0.00024334746,0.00011656112,0.000687837,0.00028767216,0.00028049859,0.00033516382,0.00019848772,0.0006701289],"category_scores_gemma":[0.00022933325,0.000097353884,0.000054638494,0.00065825,0.00015965004,0.0001501983,0.00017313904,0.00016542028,0.00015980507],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038799626,0.00011485183,0.7837386,0.00008172847,0.00005364414,0.00039661553,0.0007519625,0.0053263907,0.14016499,0.00020902281,0.0019598631,0.06681439],"study_design_scores_gemma":[0.000006430952,0.000041999836,0.98224175,0.000007619885,0.000012729607,0.000039710147,0.00036879294,0.010229307,0.006068874,0.000027780958,0.00094480213,0.000010184493],"about_ca_topic_score_codex":0.2935936,"about_ca_topic_score_gemma":0.58421904,"teacher_disagreement_score":0.2935936,"about_ca_system_score_codex":0.000875034,"about_ca_system_score_gemma":0.0010618581,"threshold_uncertainty_score":0.5837693},"labels":[],"label_agreement":null},{"id":"W4310061856","doi":"10.1029/2022jb024612","title":"Fault Slip Behaviors Modulated by Locally Increased Fluid Pressure: Earthquake Nucleation and Slow Slip Events","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"National Natural Science Foundation of China","keywords":"Slip (aerodynamics); Episodic tremor and slip; Seismology; Geology; Seismic gap; Remotely triggered earthquakes; Nucleation; Fault (geology); Engineering; Subduction; Tectonics; Physics","score_opus":0.021566967466016603,"score_gpt":0.28434478516103606,"score_spread":0.26277781769501946,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4310061856","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99248296,0.00015583212,0.004511339,0.00009030033,0.00002896808,0.000021890331,0.00020992775,0.00008366115,0.002415082],"genre_scores_gemma":[0.99915826,0.000052110026,0.00056730944,0.000010217288,0.0000038131038,0.000010086587,0.00006623963,0.000009402541,0.00012256287],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999156,0.000015568387,0.0000068759396,0.000015972775,0.000014945065,0.000031004452],"domain_scores_gemma":[0.9996208,0.00013128854,0.00011495187,0.000030467987,0.000042071213,0.0000603261],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018942513,0.00035778322,0.0004583035,0.0004163891,0.0004171336,0.00055662496,0.0004764142,0.0005880037,0.0019117822],"category_scores_gemma":[0.0011384994,0.00027284518,0.0005127765,0.00031935517,0.00062891375,0.0005013384,0.00047094782,0.00047212618,0.00011131121],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019846999,0.00023725582,0.054149956,0.00022495023,0.00015410788,0.000616547,0.00016472659,0.9079838,0.02700303,0.005046668,0.0006925107,0.00352794],"study_design_scores_gemma":[0.000035062396,0.000062382445,0.008966871,0.00000856025,0.00002533601,0.00003417347,0.000051684572,0.9880751,0.0017229621,0.0007816043,0.00022032647,0.000016026503],"about_ca_topic_score_codex":0.0064389626,"about_ca_topic_score_gemma":0.0030704048,"teacher_disagreement_score":0.0064389626,"about_ca_system_score_codex":0.00037462325,"about_ca_system_score_gemma":0.00053020474,"threshold_uncertainty_score":0.0128029585},"labels":[],"label_agreement":null},{"id":"W4311816500","doi":"10.1029/2022jb024113","title":"Geometric Control on Seismic Rupture and Earthquake Sequence Along the Yingxiu‐Beichuan Fault With Implications for the 2008 Wenchuan Earthquake","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; McGill University","funders":"National Key Research and Development Program of China","keywords":"Seismology; Geology; Slip (aerodynamics); Earthquake rupture; Strike-slip tectonics; Fault (geology); Magnetic dip; Surface rupture; Tectonics; Geodesy; Engineering; Geophysics","score_opus":0.05285330245016274,"score_gpt":0.31852828033026065,"score_spread":0.2656749778800979,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4311816500","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981481,0.00003681041,0.0011478739,0.000046089033,0.000004893365,0.0000038984517,0.000035819114,0.000015786245,0.0005608516],"genre_scores_gemma":[0.99977857,0.00001765685,0.00009758699,0.0000032243058,0.0000015657721,0.0000015314204,0.000020228103,0.0000026928114,0.000076847],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99989045,0.000021294434,0.0000063115804,0.000040032795,0.000013813869,0.00002805983],"domain_scores_gemma":[0.999729,0.000055747496,0.00010421571,0.00003223674,0.000032861364,0.000046022946],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020871747,0.00037324708,0.00040222594,0.0005082347,0.00033950014,0.0005981264,0.00039217767,0.00047676804,0.0011071512],"category_scores_gemma":[0.0009150068,0.00032429886,0.00038550587,0.00037587713,0.00059129595,0.00039579565,0.00050969236,0.00023176154,0.00008736493],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019307197,0.00014430749,0.10906552,0.00004737451,0.000097000135,0.0007515316,0.00012165614,0.8586397,0.020196427,0.0037865145,0.00030334754,0.006653482],"study_design_scores_gemma":[0.000018692113,0.000101387326,0.09635532,0.0000053158637,0.00003533156,0.0000870523,0.000090036985,0.9005469,0.0011730349,0.001372639,0.00018988819,0.000024473642],"about_ca_topic_score_codex":0.012458855,"about_ca_topic_score_gemma":0.007255022,"teacher_disagreement_score":0.012458855,"about_ca_system_score_codex":0.0009099442,"about_ca_system_score_gemma":0.00062476646,"threshold_uncertainty_score":0.024772704},"labels":[],"label_agreement":null},{"id":"W4312071137","doi":"10.1029/2022jb025517","title":"Lithospheric <i>S</i> Wave Velocity Variations Beneath the Mackenzie Mountains and Northern Canadian Cordillera","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Yukon University; Geological Survey of Canada; Natural Resources Canada; University of Calgary; University of Ottawa","funders":"National Science Foundation","keywords":"Geology; Lithosphere; Seismology; Crust; Induced seismicity; Craton; Tectonics; Plate tectonics; Seismic tomography; Thrust fault; Mantle (geology); Geophysics","score_opus":0.03051684050892847,"score_gpt":0.2698213976719133,"score_spread":0.23930455716298485,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4312071137","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972072,0.00015412775,0.000040588846,0.0000616459,0.000002251593,0.0000049379896,0.0004965126,0.000016084054,0.0020165876],"genre_scores_gemma":[0.9991159,0.00006158855,0.000110544155,0.000010303607,0.0000015789705,0.0000023654377,0.00025608725,0.000002857102,0.0004389337],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998883,0.0000031047825,0.000004573961,0.00003282541,0.000029573637,0.00004166854],"domain_scores_gemma":[0.9997892,0.000008933987,0.000035793662,0.000009834906,0.00011362116,0.000042686595],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000119989476,0.00030759582,0.00020091259,0.0014318438,0.0014691617,0.0008488375,0.00048030043,0.00018740175,0.0021609107],"category_scores_gemma":[0.00040553202,0.00012976452,0.00013656297,0.0013646914,0.00047161247,0.00019855399,0.0005397998,0.00017409821,0.00015783307],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001917524,0.000026354806,0.95666564,0.00004729744,0.00009389333,0.00024804642,0.0014261717,0.0011012008,0.013747037,0.00044538657,0.001617483,0.02438959],"study_design_scores_gemma":[0.0000027294313,0.0000029851815,0.99834716,0.00000655662,0.000007474546,0.0000135982045,0.00039705628,0.00036527173,0.00020654629,0.000013986881,0.0006309669,0.000005743003],"about_ca_topic_score_codex":0.97631943,"about_ca_topic_score_gemma":0.98871803,"teacher_disagreement_score":0.97631943,"about_ca_system_score_codex":0.0052831355,"about_ca_system_score_gemma":0.0037613572,"threshold_uncertainty_score":0.047640026},"labels":[],"label_agreement":null},{"id":"W4312156228","doi":"10.1029/2022jb024991","title":"Constraints on Secular Geocenter Velocity From Absolute Gravity Observations in Central North America: Implications for Global Melting Rates","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geodesy; Post-glacial rebound; Secular variation; Climatology; Global Positioning System; Geology; Series (stratigraphy); Glacial period; Geophysics; Geomorphology","score_opus":0.0920475741316496,"score_gpt":0.3380890574064577,"score_spread":0.24604148327480813,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4312156228","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99758744,0.00029578933,0.00038206467,0.00005176619,0.000005447766,0.0000028575398,0.0004554004,0.00001775818,0.0012014279],"genre_scores_gemma":[0.9992736,0.000059844406,0.00023124382,0.000008042611,0.000002714587,0.0000024457242,0.00033582782,0.0000046287482,0.00008172502],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981743,0.000040857638,0.000014626764,0.00006081851,0.000029860317,0.000036342517],"domain_scores_gemma":[0.99902916,0.00020009001,0.00029221768,0.00009689304,0.00030083655,0.00008083558],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008993941,0.0002691805,0.00024792048,0.0014040231,0.00038094205,0.0007805348,0.00035101036,0.00023730607,0.00082043034],"category_scores_gemma":[0.002320421,0.0002084754,0.0001715825,0.0018226425,0.0004526931,0.00052993314,0.00046478442,0.0001983237,0.00010789616],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000084266205,0.000013575644,0.97945935,0.00003274841,0.00006662078,0.00005424616,0.00033424425,0.0021060307,0.006627431,0.00016842452,0.000322195,0.010730865],"study_design_scores_gemma":[0.00000249148,0.0000047303797,0.99811363,0.0000084920985,0.000008860559,0.000013382542,0.00012835748,0.0011149892,0.00027598164,0.000044733086,0.00028041465,0.000003817401],"about_ca_topic_score_codex":0.18590671,"about_ca_topic_score_gemma":0.32877943,"teacher_disagreement_score":0.8140933,"about_ca_system_score_codex":0.0009330307,"about_ca_system_score_gemma":0.0008390445,"threshold_uncertainty_score":0.36964923},"labels":[],"label_agreement":null},{"id":"W4313575804","doi":"10.1029/2022jb025772","title":"Formation of Tarim Large Igneous Province and Strengthened Lithosphere Revealed Through Machine Learning","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"Fundamental Research Funds for the Central Universities; National Natural Science Foundation of China","keywords":"Geology; Magmatism; Lithosphere; Basalt; Subduction; Igneous rock; Mafic; Mantle (geology); Large igneous province; Geochemistry; Mantle plume; Earth science; Crust; Petrology; Tectonics; Seismology","score_opus":0.031466138517196825,"score_gpt":0.2948128812373586,"score_spread":0.2633467427201618,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4313575804","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99725986,0.00009005641,0.001768217,0.00005939652,0.000004119214,0.0000035929688,0.00019812705,0.000062956984,0.00055358023],"genre_scores_gemma":[0.99913293,0.000025059991,0.00049639965,0.0000041278086,0.0000029227647,0.0000013551812,0.00023304556,0.0000036793967,0.00010052323],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999263,0.000010989578,0.000004858445,0.00002683663,0.000012322283,0.000018720948],"domain_scores_gemma":[0.99982977,0.000033322107,0.00005237251,0.000024291732,0.00003397534,0.000026340027],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029854677,0.00025005202,0.00020698436,0.0012456937,0.00023234099,0.00049588585,0.00025539694,0.00022453602,0.0006762584],"category_scores_gemma":[0.00049812737,0.00011029647,0.00030601514,0.0008519876,0.0003151324,0.00031973416,0.00034063714,0.00023704125,0.00013731483],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014152064,0.00006761472,0.864752,0.00007081132,0.00014830612,0.0005134535,0.00017193411,0.078709684,0.023693163,0.0013215797,0.00075788074,0.02965207],"study_design_scores_gemma":[0.000012849158,0.00003473706,0.42234403,0.000014732252,0.00006144324,0.00010579236,0.00021469886,0.5692341,0.0057477,0.001350852,0.0008622833,0.000016794413],"about_ca_topic_score_codex":0.015637629,"about_ca_topic_score_gemma":0.016681762,"teacher_disagreement_score":0.015637629,"about_ca_system_score_codex":0.0004709312,"about_ca_system_score_gemma":0.00041724838,"threshold_uncertainty_score":0.03109324},"labels":[],"label_agreement":null},{"id":"W4315782240","doi":"10.1029/2022jb025388","title":"Discovery of a &gt;1,000 km Cambrian Eclogite‐Bearing High‐Pressure Metamorphic Belt in the Central Asian Orogenic Belt: Implications for the Final Closure of the Pan‐Rodinian Ocean","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval; University of British Columbia","funders":"National Natural Science Foundation of China","keywords":"Eclogite; Protolith; Geology; Geochemistry; Metamorphic facies; Gneiss; Zircon; Metamorphic rock; Metamorphism; Continental arc; Petrology; Geothermobarometry; Subduction; Paleontology; Facies; Tectonics; Volcanic rock","score_opus":0.05451680633562835,"score_gpt":0.30192277009381535,"score_spread":0.247405963758187,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4315782240","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99912375,0.00010378922,0.00010248919,0.000016536105,0.000001097828,0.0000030179808,0.0000812573,0.0000083988525,0.0005596723],"genre_scores_gemma":[0.99944943,0.00004126229,0.00015490627,0.000008903381,0.0000015421437,0.0000020255366,0.00016491573,0.0000036216281,0.0001735179],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993634,0.0000031175805,0.0000033937913,0.000029239336,0.000011908642,0.000016044492],"domain_scores_gemma":[0.9998801,0.00000924113,0.00004395745,0.000014954229,0.000026547343,0.000025112618],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016903285,0.00017685033,0.00013026154,0.0007629472,0.00052374846,0.0006317532,0.00026755527,0.00026690503,0.0010607191],"category_scores_gemma":[0.00017475383,0.0001549571,0.00014629702,0.00057616923,0.00037444205,0.00018258288,0.00042988182,0.00019086174,0.00016544346],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000112141955,0.000019602727,0.88783455,0.000037478578,0.00003705247,0.00051374285,0.0008107561,0.00017596682,0.100680605,0.00028548564,0.00007999655,0.009412675],"study_design_scores_gemma":[0.0000036002525,0.0000156112,0.99659294,0.000004684933,0.00000925467,0.00013016837,0.00018522193,0.00026589568,0.0019517847,0.000022546044,0.0008164578,0.0000018019771],"about_ca_topic_score_codex":0.017289381,"about_ca_topic_score_gemma":0.019409014,"teacher_disagreement_score":0.017289381,"about_ca_system_score_codex":0.0006638938,"about_ca_system_score_gemma":0.0002549799,"threshold_uncertainty_score":0.034377456},"labels":[],"label_agreement":null},{"id":"W4315784240","doi":"10.1029/2022jb025048","title":"Quantitative Evaluation of the Competing Effects of Wastewater Disposal and Hydraulic Fracturing on Causing Induced Earthquakes: A Case Study of an M3.1 Earthquake Sequence in Western Canada","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geoscience BC; Ocean Networks Canada Society; University of Victoria; Geological Survey of Canada","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; McGill University","keywords":"Geology; Hydraulic fracturing; Seismology; Pore water pressure; Perturbation (astronomy); Structural basin; Poromechanics; Geotechnical engineering; Paleontology; Physics","score_opus":0.10674662721159774,"score_gpt":0.378138658603342,"score_spread":0.2713920313917443,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4315784240","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99850684,0.00004824863,0.00048763744,0.000018376919,0.0000012738216,0.000022927486,0.00039426563,0.00001797707,0.0005024572],"genre_scores_gemma":[0.99842536,0.000047622092,0.0009227233,0.0000044499993,0.0000016672498,0.0000050653753,0.00038218708,0.0000034340428,0.00020745165],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99973077,0.000029232266,0.000019414181,0.000037016216,0.00010717761,0.0000764481],"domain_scores_gemma":[0.9988881,0.000420426,0.00017694797,0.000063614876,0.00031089116,0.00014002557],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00046047027,0.00044971093,0.0003564984,0.0020683755,0.00060940685,0.0006910138,0.0005701608,0.0004084683,0.00064762693],"category_scores_gemma":[0.0018062845,0.00018244504,0.00040966645,0.002586627,0.00059058005,0.00029412704,0.00041870246,0.0002280307,0.00005742137],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021640141,0.00021619082,0.86308146,0.00019689092,0.00021655521,0.004803572,0.0009152092,0.09265631,0.0110792825,0.0010000477,0.0006501811,0.02496793],"study_design_scores_gemma":[0.000020802674,0.00008059668,0.8440333,0.0000199727,0.00011537621,0.0003415789,0.0019836265,0.14958268,0.0027158519,0.00020710954,0.00086650584,0.000032580243],"about_ca_topic_score_codex":0.68208814,"about_ca_topic_score_gemma":0.7935473,"teacher_disagreement_score":0.31791186,"about_ca_system_score_codex":0.0035214082,"about_ca_system_score_gemma":0.002349536,"threshold_uncertainty_score":0.6395682},"labels":[],"label_agreement":null},{"id":"W4318191475","doi":"10.1029/2022jb025034","title":"Rapid Tremor Migration During Few Minute‐Long Slow Earthquakes in Cascadia","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Seismology; Episodic tremor and slip; Geology; Slip (aerodynamics); Subduction; Coherence (philosophical gambling strategy); Geodesy; Tectonics; Physics","score_opus":0.05701483990482568,"score_gpt":0.3162004412671169,"score_spread":0.2591856013622912,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4318191475","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994048,0.000029938508,0.000063278596,0.000018048713,0.0000010298977,0.0000017715856,0.000107819906,0.000009509353,0.00036388525],"genre_scores_gemma":[0.9997316,0.000021103555,0.000043356806,0.000003060316,0.0000013348483,0.0000018380474,0.00009329619,0.0000020447899,0.000102324506],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999299,0.000008550931,0.000005482181,0.000020408515,0.000018448147,0.000017209706],"domain_scores_gemma":[0.999395,0.00009292723,0.00019946242,0.000040887528,0.0001223947,0.00014935769],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001771026,0.00017782209,0.00018877855,0.0012277167,0.00044820856,0.0003799559,0.00019789021,0.00025509883,0.0012450491],"category_scores_gemma":[0.00094529707,0.0001693791,0.00011510151,0.0009915016,0.00033274954,0.00019536281,0.0005044761,0.00019095751,0.00023508962],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019213714,0.000042445205,0.9609338,0.000051220082,0.00006295036,0.00045081906,0.0016589429,0.0011882639,0.027978517,0.000102749495,0.00035991584,0.006978322],"study_design_scores_gemma":[0.0000021996514,0.0000160391,0.999236,0.0000019192141,0.0000037666446,0.000035090394,0.00021034769,0.00024518886,0.00012757661,0.000014091087,0.0001054871,0.000002304362],"about_ca_topic_score_codex":0.036346883,"about_ca_topic_score_gemma":0.06284465,"teacher_disagreement_score":0.9636531,"about_ca_system_score_codex":0.0005186746,"about_ca_system_score_gemma":0.00026838252,"threshold_uncertainty_score":0.07227063},"labels":[],"label_agreement":null},{"id":"W4319067165","doi":"10.1029/2022jb025955","title":"Combining Paleomagnetic and Re‐Os Isotope Data to Date Hydrocarbon Generation and Accumulation Processes","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Lakehead University","funders":"National Natural Science Foundation of China; National Science Foundation","keywords":"Paleomagnetism; Geology; Cretaceous; Paleontology; Permian; Tectonics; Radiometric dating; Source rock; Hydrocarbon exploration; Carbonate; Geochemistry","score_opus":0.17674823171571438,"score_gpt":0.38876993910244456,"score_spread":0.21202170738673018,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4319067165","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9802768,0.0010908975,0.012915685,0.000045201417,0.000040905576,0.000026746826,0.0005625029,0.0001426218,0.0048987456],"genre_scores_gemma":[0.98867375,0.00049682276,0.008974528,0.000022932334,0.000021129903,0.00001274399,0.00037348535,0.00005362913,0.0013710653],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99982893,0.000012552334,0.000014958214,0.00006131124,0.000058041674,0.000024064502],"domain_scores_gemma":[0.99969935,0.00002529328,0.00011006606,0.000041019237,0.000101019825,0.000023149098],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005262132,0.00054264715,0.00029535135,0.002600134,0.00022492449,0.0006010769,0.00036765035,0.00034356915,0.0008283269],"category_scores_gemma":[0.0004490549,0.0002732351,0.00022773106,0.0015318322,0.0003682732,0.0006591144,0.00052241056,0.00028222075,0.0003422502],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029790268,0.000040508057,0.1929971,0.00018575916,0.0001944166,0.0002758066,0.00023046011,0.0024284204,0.754693,0.00054268853,0.00020191714,0.047912024],"study_design_scores_gemma":[0.000034794903,0.00025084245,0.51940614,0.000059132093,0.00041022562,0.0008972533,0.00043066536,0.03681278,0.4274042,0.0009290163,0.013267351,0.00009768872],"about_ca_topic_score_codex":0.0040682578,"about_ca_topic_score_gemma":0.011162689,"teacher_disagreement_score":0.0040682578,"about_ca_system_score_codex":0.00035300993,"about_ca_system_score_gemma":0.00035056873,"threshold_uncertainty_score":0.008089125},"labels":[],"label_agreement":null},{"id":"W4319602865","doi":"10.1029/2022jb025662","title":"A Long‐Term Earthquake Catalog for the Endeavour Segment: Constraints on the Extensional Cycle and Evidence for Hydrothermal Venting Supported by Propagating Rifts","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada; Ocean Networks Canada Society; University of Victoria","funders":"National Defense Science and Engineering Graduate; National Science Foundation","keywords":"Geology; Seismology; Induced seismicity; Seismometer; Rift; Ridge; Magmatism; Bathymetry; Observatory; Mid-ocean ridge; Geophysics; Tectonics; Paleontology; Oceanography","score_opus":0.10001777294504052,"score_gpt":0.3574782625628935,"score_spread":0.25746048961785295,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4319602865","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99345917,0.00006614999,0.0002670761,0.00002222498,0.0000021231479,0.000011685,0.005028549,0.000025122792,0.0011179814],"genre_scores_gemma":[0.9852769,0.00006402788,0.0006734936,0.000009185334,0.0000076751385,0.000014873822,0.013553435,0.00000960763,0.00039086302],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99977595,0.000021077558,0.000030121346,0.00004780645,0.000070132,0.000054943397],"domain_scores_gemma":[0.998125,0.00014441146,0.00068025675,0.00022222071,0.00048493742,0.0003431601],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003746972,0.00019451746,0.00021608475,0.0026112502,0.00032555498,0.00057246175,0.00030424702,0.00019022169,0.0011942049],"category_scores_gemma":[0.0013517966,0.00011536072,0.00020596146,0.0024422004,0.00022118325,0.0003387817,0.0007046124,0.00014298651,0.00037729103],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000022810476,0.0000123965665,0.9908308,0.000014957492,0.000017258628,0.000092807175,0.00015090767,0.0002859543,0.0029943243,0.00003880141,0.00030688016,0.0052321474],"study_design_scores_gemma":[0.0000017268734,0.0000070461037,0.99897003,0.0000038807175,0.000003794912,0.000031768046,0.00008198648,0.00031160566,0.00014735304,0.000009228019,0.0004294752,0.0000022173028],"about_ca_topic_score_codex":0.06463119,"about_ca_topic_score_gemma":0.15774573,"teacher_disagreement_score":0.06463119,"about_ca_system_score_codex":0.00048842013,"about_ca_system_score_gemma":0.0006515821,"threshold_uncertainty_score":0.12851},"labels":[],"label_agreement":null},{"id":"W4320879407","doi":"10.1029/2022jb025809","title":"Experimental Measurement of Enhanced and Hindered Particle Settling in Turbulent Gas‐Particle Suspensions, and Geophysical Implications","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Particle Dynamics in Fluid Flows","field":"Engineering","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Institute for Advanced Research; Kavli Institute for Theoretical Physics, University of California, Santa Barbara; Agence Nationale de la Recherche; National Science Foundation","keywords":"Settling; Particle (ecology); Turbulence; Drag; Mechanics; Particle velocity; Drag coefficient; Materials science; Mineralogy; Chemistry; Physics; Geology; Thermodynamics","score_opus":0.06619093333015237,"score_gpt":0.35328216321416855,"score_spread":0.2870912298840162,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4320879407","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99608827,0.00008690305,0.003361546,0.000019566198,0.000010106935,0.000009948505,0.000050870007,0.000029097995,0.00034370855],"genre_scores_gemma":[0.9976998,0.000043816908,0.0020340884,0.000010632592,0.0000035654925,0.000008510122,0.000058585934,0.000005732359,0.0001352658],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9997725,0.000042613196,0.000019606847,0.00005654324,0.00007999291,0.000028666911],"domain_scores_gemma":[0.9994398,0.00028207793,0.0000829867,0.000037528986,0.00010898672,0.000048545277],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040401463,0.0002722797,0.00016744074,0.00030682902,0.00040780692,0.00037007406,0.0002960034,0.00040219352,0.00052777387],"category_scores_gemma":[0.0009718529,0.00015501001,0.00011164415,0.00022683087,0.0005201036,0.00027666969,0.00034026892,0.000435011,0.00008965155],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010762915,0.000039722992,0.002179003,0.000024150817,0.00000469986,0.000030609808,0.0000661794,0.0006255222,0.9955799,0.00013080584,0.000029621764,0.0011821223],"study_design_scores_gemma":[0.000027196995,0.00046539138,0.0099588465,0.0000066848347,0.000010787578,0.000050986393,0.000085142194,0.012015395,0.97691464,0.00012610448,0.0003236758,0.00001505032],"about_ca_topic_score_codex":0.0012699715,"about_ca_topic_score_gemma":0.0009183659,"teacher_disagreement_score":0.0012699715,"about_ca_system_score_codex":0.0002683229,"about_ca_system_score_gemma":0.00016018373,"threshold_uncertainty_score":0.0025252104},"labels":[],"label_agreement":null},{"id":"W4320917205","doi":"10.1029/2022jb025050","title":"Beamforming of Rayleigh and Love Waves in the Course of Atlantic Cyclones","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Deutsche Forschungsgemeinschaft","keywords":"Microseism; Geology; Seismometer; Rayleigh wave; Seismology; Love wave; Geophysics; Seismogram; Wind wave; Typhoon; Storm; Surface wave; Wave propagation; Climatology; Oceanography; Physics; Mechanical wave; Longitudinal wave","score_opus":0.0388562789201129,"score_gpt":0.3313060886154112,"score_spread":0.2924498096952983,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4320917205","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954465,0.000040897627,0.003418512,0.00002196093,0.0000062333456,0.0000068028803,0.0001805855,0.000026273368,0.0008520896],"genre_scores_gemma":[0.99733305,0.000054232114,0.0017410805,0.000004961641,0.000005826733,0.0000046523082,0.00028179277,0.000008726947,0.00056584366],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999361,0.0000075986236,0.0000021701248,0.000014485427,0.000014352867,0.00002530214],"domain_scores_gemma":[0.9998529,0.00003562617,0.00002550394,0.000007836419,0.00005178893,0.000026227512],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010940432,0.00029813946,0.00012958226,0.0005844694,0.00013926973,0.00029999478,0.00008666635,0.000112313544,0.0007649963],"category_scores_gemma":[0.00051503663,0.0001503307,0.00016225825,0.0004401531,0.00013428101,0.00016051458,0.00017001128,0.000119221455,0.00019669773],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008120083,0.00010629028,0.17436312,0.00007447779,0.000102655824,0.0006420317,0.0006869069,0.031154988,0.6644535,0.0009902995,0.0011035079,0.12551026],"study_design_scores_gemma":[0.000014875519,0.00011838028,0.9178595,0.000010896289,0.000038521874,0.00017598335,0.00043408526,0.059955504,0.020593993,0.00021898495,0.00054839224,0.000030883963],"about_ca_topic_score_codex":0.008829017,"about_ca_topic_score_gemma":0.01605046,"teacher_disagreement_score":0.008829017,"about_ca_system_score_codex":0.00016026072,"about_ca_system_score_gemma":0.00028997473,"threshold_uncertainty_score":0.017555296},"labels":[],"label_agreement":null},{"id":"W4321327328","doi":"10.1029/2022jb025964","title":"Implicit Seismic Full Waveform Inversion With Deep Neural Representation","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":75,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Ocean University of China; China Postdoctoral Science Foundation","keywords":"Initialization; Inversion (geology); Inference; Computer science; Algorithm; Inverse problem; Geophysical imaging; Seismic inversion; Deep learning; Bayesian inference; Waveform; Artificial neural network; Bayesian probability; Artificial intelligence; Geology; Geophysics; Seismology; Mathematics; Data assimilation; Meteorology; Telecommunications","score_opus":0.04148452149159892,"score_gpt":0.3250095647305852,"score_spread":0.28352504323898625,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321327328","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.027841028,0.00007915498,0.9692947,0.00022126938,0.000022714603,0.000019653538,0.00010515414,0.0006102887,0.0018059679],"genre_scores_gemma":[0.6505067,0.00011475122,0.34483188,0.00013527293,0.000036685055,0.000079529826,0.0005082073,0.00016341884,0.0036235987],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99985886,0.00004192177,0.000008372001,0.00002318779,0.00004828397,0.0000193805],"domain_scores_gemma":[0.99943846,0.00027719344,0.000057904643,0.00009482871,0.00010314697,0.000028437682],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00060924946,0.0005396787,0.0003271907,0.0002848029,0.00013976889,0.00065005623,0.0010166009,0.00071479427,0.0018251765],"category_scores_gemma":[0.002461269,0.00036088322,0.00034884413,0.00039493424,0.0004077725,0.0014054192,0.0010652072,0.0014832442,0.00047188837],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006288828,0.00002938796,0.0004307666,0.000037277627,0.000021739617,0.000032902943,0.000030476747,0.912936,0.0050691627,0.009831444,0.0008129101,0.07070497],"study_design_scores_gemma":[0.000001312819,0.0000031164423,0.00001861123,0.0000011165534,5.2016543e-7,0.0000021459089,9.94816e-7,0.99844605,0.00033836567,0.0011068037,0.000079988786,0.0000010144835],"about_ca_topic_score_codex":0.004249566,"about_ca_topic_score_gemma":0.0055111214,"teacher_disagreement_score":0.004249566,"about_ca_system_score_codex":0.00041496058,"about_ca_system_score_gemma":0.00092140376,"threshold_uncertainty_score":0.008449674},"labels":[],"label_agreement":null},{"id":"W4321329740","doi":"10.1029/2022jb025344","title":"Stress Features Inferred From Induced Earthquakes in the Weiyuan Shale Gas Block in Southwestern China","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Chinese Academy of Sciences; National Natural Science Foundation of China","keywords":"Geology; Seismology; Focal mechanism; Hydraulic fracturing; Stress field; Tectonics; Slip (aerodynamics); Shale gas; Stress (linguistics); Oil shale; Geotechnical engineering; Paleontology","score_opus":0.056071101433650065,"score_gpt":0.3287549339407007,"score_spread":0.27268383250705064,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321329740","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997521,0.000010856753,0.000048814152,0.0000053933877,5.753737e-7,0.0000016429902,0.00007803783,0.000004966433,0.00009759409],"genre_scores_gemma":[0.9997218,0.000010961614,0.000046298992,0.0000017689108,0.0000012982136,0.0000019607694,0.0001560786,7.797773e-7,0.00005905061],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999304,0.000005630739,0.000008811985,0.000016907503,0.000017217759,0.000021030635],"domain_scores_gemma":[0.99977416,0.000022175316,0.00006488193,0.000017875487,0.000054858796,0.00006619216],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001390028,0.0002727825,0.00018365985,0.0012226233,0.00032412022,0.0002692154,0.00022413731,0.00022677012,0.00043688025],"category_scores_gemma":[0.00033371022,0.00015680329,0.00016592737,0.0010945101,0.00021341881,0.0001706105,0.0002932498,0.000095219315,0.00008095815],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007249757,0.000038012444,0.97564906,0.000030532094,0.000038239257,0.00046479198,0.00044967886,0.0028015058,0.011907364,0.000075536234,0.00017900471,0.008293917],"study_design_scores_gemma":[0.0000027785027,0.000011802629,0.99708587,0.0000018499746,0.0000074475533,0.000024069212,0.000107603584,0.0024560771,0.00022130807,0.000011214957,0.00006727434,0.0000026795365],"about_ca_topic_score_codex":0.041921254,"about_ca_topic_score_gemma":0.06436471,"teacher_disagreement_score":0.041921254,"about_ca_system_score_codex":0.00046961932,"about_ca_system_score_gemma":0.00044749843,"threshold_uncertainty_score":0.08335447},"labels":[],"label_agreement":null},{"id":"W4321444310","doi":"10.1029/2022jb024813","title":"Recovery of the Alberta Basin Sedimentary Structures in Southern‐Central Alberta Using Nonlinear Inversions of Receiver Functions","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Alberta","funders":"","keywords":"Geology; Sedimentary rock; Seismology; Sedimentary basin; Structural basin; Inversion (geology); Geomorphology; Paleontology","score_opus":0.037740540336815724,"score_gpt":0.29900651078115276,"score_spread":0.261265970444337,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321444310","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9933298,0.000027989998,0.0045823553,0.0000490401,0.0000038234793,0.0000062010795,0.00032899278,0.00016808981,0.0015037421],"genre_scores_gemma":[0.99697125,0.000015764746,0.0021992966,0.0000040351615,9.553039e-7,0.000001990861,0.0002554559,0.000013476101,0.00053764554],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99995077,0.0000045342454,0.0000013401467,0.000008966315,0.000018322096,0.000016054353],"domain_scores_gemma":[0.99991167,0.000012581513,0.000012476998,0.0000074572717,0.00004233972,0.000013494235],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001264278,0.0003869215,0.000112431415,0.00045314076,0.0003538808,0.00045470087,0.00046540314,0.0002209697,0.00093524146],"category_scores_gemma":[0.00043229715,0.0002038864,0.00015589819,0.0005044018,0.00024651308,0.00014842804,0.00021828743,0.00020001193,0.00017015074],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003414398,0.00009946135,0.19593377,0.000055484852,0.00009228476,0.00040120236,0.0004936723,0.67552024,0.04395247,0.001506085,0.0014165824,0.08018736],"study_design_scores_gemma":[0.000029009027,0.000020204418,0.13077766,0.000007802999,0.000018493993,0.000025446758,0.00018226668,0.8642725,0.0035236087,0.00026177833,0.00086003414,0.000021208321],"about_ca_topic_score_codex":0.72752863,"about_ca_topic_score_gemma":0.7887307,"teacher_disagreement_score":0.27247137,"about_ca_system_score_codex":0.0022675646,"about_ca_system_score_gemma":0.0032483342,"threshold_uncertainty_score":0.54815197},"labels":[],"label_agreement":null},{"id":"W4322504397","doi":"10.1029/2022jb025745","title":"A New P‐Wave Tomographic Model (CAP22) for North America: Implications for the Subduction and Cratonic Metasomatic Modification History of Western Canada and Alaska","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Ottawa; Geological Survey of Canada; Université du Québec à Montréal","funders":"HORIZON EUROPE European Research Council; Natural Environment Research Council; Sight Research UK","keywords":"Subduction; Geology; Craton; Seismology; Plate tectonics; Archean; Mantle (geology); Proterozoic; Seismometer; Volcanism; Crust; Tectonics; Intraplate earthquake; Paleontology","score_opus":0.08177245085894629,"score_gpt":0.30841789958218024,"score_spread":0.22664544872323394,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4322504397","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.84129643,0.00046362108,0.1230343,0.00077036605,0.00009898968,0.00018127637,0.007140186,0.0023277656,0.024687042],"genre_scores_gemma":[0.9444134,0.00018207236,0.047867842,0.000068633584,0.000021086698,0.00011034593,0.0028813472,0.00023991117,0.004215324],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992085,0.00000809002,0.0000033213537,0.000031619446,0.000020874775,0.000015196415],"domain_scores_gemma":[0.99981946,0.000028535746,0.000015065761,0.000013643556,0.00009314551,0.000030184456],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016856352,0.0006750437,0.00030791532,0.00070623396,0.0008641721,0.0014841578,0.0015777203,0.000780501,0.0025047448],"category_scores_gemma":[0.0007607399,0.00039362343,0.00051748723,0.0010934831,0.00045782054,0.00053339615,0.00042099901,0.00049548637,0.000330681],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000035465335,0.000021821219,0.011086503,0.000018358827,0.00004713271,0.00007313317,0.0000617236,0.9766341,0.0010810399,0.0011064422,0.001318857,0.008515534],"study_design_scores_gemma":[0.000009676572,0.0000031628063,0.002145817,0.0000034640727,0.00000982234,0.0000113077085,0.000033256514,0.996305,0.000115581424,0.00034933502,0.0010056389,0.000007984806],"about_ca_topic_score_codex":0.77007425,"about_ca_topic_score_gemma":0.7193459,"teacher_disagreement_score":0.22992575,"about_ca_system_score_codex":0.0030831483,"about_ca_system_score_gemma":0.0054221763,"threshold_uncertainty_score":0.46255964},"labels":[],"label_agreement":null},{"id":"W4322735239","doi":"10.1029/2022jb024985","title":"Complex 3‐D Surface Deformation in the 1971 San Fernando, California Earthquake Reveals Static and Dynamic Controls on Off‐Fault Deformation","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Canada Foundation for Innovation; Natural Sciences and Engineering Research Council of Canada; Centre National d’Etudes Spatiales; Southern California Earthquake Center","keywords":"Fault trace; Geology; Slip (aerodynamics); Seismology; Thrust fault; Fault (geology); Strike-slip tectonics; Geodesy; Thrust; Rake angle; Rake; Deformation (meteorology); Geometry; Geomorphology; Materials science; Engineering","score_opus":0.05692740955110933,"score_gpt":0.3371822339417742,"score_spread":0.2802548243906649,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4322735239","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99887675,0.000014722615,0.000048511178,0.000012613315,0.0000012971249,0.0000016716949,0.00028354788,0.000011828192,0.0007489377],"genre_scores_gemma":[0.9994772,0.000015512973,0.00005741101,0.00000293743,0.0000014521889,0.0000011960609,0.00029330185,0.0000035543956,0.00014736713],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996424,0.0000021594235,0.0000012979019,0.000009592631,0.000009769037,0.000012909636],"domain_scores_gemma":[0.9999205,0.00001291135,0.000021045757,0.000007775308,0.000016768134,0.0000209452],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000061257546,0.00015945711,0.000158961,0.0006448332,0.00031305692,0.0003844117,0.00012168139,0.00022197654,0.0010869561],"category_scores_gemma":[0.00027757883,0.0001519494,0.00015017139,0.000661045,0.00023096321,0.0001800213,0.00021901082,0.00017233641,0.00016479874],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006101747,0.00017620473,0.91015506,0.00004226615,0.00005980428,0.00087554706,0.0007289903,0.018877063,0.03755086,0.00028360393,0.0022025467,0.02843792],"study_design_scores_gemma":[0.000002375858,0.0000052038267,0.9981493,0.0000010568021,0.0000018787343,0.000013821558,0.000056846082,0.0015352301,0.00013067824,0.000011627403,0.00008965073,0.000002388159],"about_ca_topic_score_codex":0.08890343,"about_ca_topic_score_gemma":0.1393742,"teacher_disagreement_score":0.08890343,"about_ca_system_score_codex":0.0006974476,"about_ca_system_score_gemma":0.00026064552,"threshold_uncertainty_score":0.17677188},"labels":[],"label_agreement":null},{"id":"W4323544766","doi":"10.1029/2022jb025287","title":"Heterogeneity Versus Anisotropy and the State of Stress in Stable Cratons: Observations From a Deep Borehole in Northeastern Alberta, Canada","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Anisotropy; Borehole; Stress field; Breakout; Azimuth; Seismology; Craton; Monte Carlo method; Slip (aerodynamics); Geophysics; Geometry; Petrology; Geotechnical engineering; Physics; Tectonics","score_opus":0.052466438501888514,"score_gpt":0.2975603682532464,"score_spread":0.24509392975135788,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4323544766","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99873596,0.00006757217,0.00007370139,0.000020759368,0.0000010223624,0.000006479925,0.0003501176,0.000008106059,0.0007362927],"genre_scores_gemma":[0.9990576,0.000072353774,0.00013894541,0.000008688222,0.000001170714,0.0000027834394,0.00022326417,0.0000025580134,0.00049271225],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998338,0.000004377914,0.000005896181,0.000027537071,0.00007055388,0.000057822846],"domain_scores_gemma":[0.9995468,0.000029643039,0.00006943945,0.000013464994,0.00021829543,0.00012225463],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014815216,0.0003325678,0.0002443912,0.001862563,0.001711393,0.0009240694,0.000735,0.00031335224,0.00085648074],"category_scores_gemma":[0.0004597025,0.00029332977,0.00015958701,0.0020131932,0.0010862874,0.00021766809,0.00051884894,0.000271538,0.00016391235],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014269243,0.00004422244,0.97459376,0.000030218174,0.000034494147,0.0005065831,0.0022362305,0.00080002606,0.012432184,0.00011122907,0.000322792,0.008745686],"study_design_scores_gemma":[0.0000026662494,0.000007059965,0.9981699,0.000005783476,0.000004946878,0.00003799795,0.000900529,0.0003606911,0.00024018879,0.000011057412,0.00025376977,0.000005315847],"about_ca_topic_score_codex":0.97406536,"about_ca_topic_score_gemma":0.9928048,"teacher_disagreement_score":0.025934637,"about_ca_system_score_codex":0.008197274,"about_ca_system_score_gemma":0.0047153407,"threshold_uncertainty_score":0.05947572},"labels":[],"label_agreement":null},{"id":"W4323666345","doi":"10.1029/2022jb025957","title":"Nanoindentation of Horn River Basin Shales: The Micromechanical Contrast Between Overburden and Reservoir Formations","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Rock Mechanics and Modeling","field":"Engineering","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Geology; Bed; Nanoindentation; Overburden; Mineralogy; Anisotropy; Oil shale; Quartz; Porosimetry; Porosity; Materials science; Geotechnical engineering; Composite material; Porous medium","score_opus":0.049958669665174205,"score_gpt":0.3303957282036984,"score_spread":0.2804370585385242,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4323666345","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984041,0.0000731255,0.0008892255,0.000008004529,0.0000012734718,0.0000057573907,0.00017494465,0.000016979526,0.00042654722],"genre_scores_gemma":[0.9986172,0.00003427417,0.0008227418,0.0000088084325,7.7362176e-7,0.0000038187663,0.00012760329,0.0000045409643,0.0003803503],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999273,0.0000037793359,0.0000029095415,0.000016636455,0.00003506929,0.000014386698],"domain_scores_gemma":[0.99979895,0.00004170103,0.000028396873,0.00001365391,0.00008713334,0.000030266563],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016247004,0.00016207331,0.00011375667,0.00074146315,0.00036780178,0.00025914714,0.0002064642,0.00015482122,0.0012030728],"category_scores_gemma":[0.00022120285,0.00010735858,0.000068155154,0.00036071503,0.00033024748,0.0001314909,0.00014807901,0.00014375153,0.00014020965],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011479311,0.000029819867,0.06076698,0.000055910332,0.000017819133,0.00030503992,0.00076144,0.0013798347,0.92446977,0.00006984728,0.000113311486,0.011915367],"study_design_scores_gemma":[0.0000039622328,0.00007260687,0.8680331,0.000010076779,0.000009810616,0.00023736981,0.0009917521,0.0065700053,0.12295575,0.00004700624,0.0010546284,0.000013936091],"about_ca_topic_score_codex":0.04483314,"about_ca_topic_score_gemma":0.14751993,"teacher_disagreement_score":0.9551669,"about_ca_system_score_codex":0.00037850023,"about_ca_system_score_gemma":0.00026569373,"threshold_uncertainty_score":0.08914435},"labels":[],"label_agreement":null},{"id":"W4360951939","doi":"10.1029/2022jb025514","title":"Evidence of Vertical Slab Tearing in the Late Triassic Qinling Orogen (Central China) From Multiproxy Geochemical and Isotopic Imaging","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Beijing Nova Program; Australian Research Council; National Natural Science Foundation of China","keywords":"Geology; Subduction; Slab; Magmatism; Slab window; Lithosphere; Asthenosphere; Tearing; Seismology; Geophysics; Geochemistry; Petrology; Tectonics; Oceanic crust","score_opus":0.05827918726037028,"score_gpt":0.3195598000647816,"score_spread":0.2612806128044113,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4360951939","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99907553,0.00014660967,0.00025195608,0.00001433406,0.0000017073647,0.000003873599,0.00011490341,0.000009971121,0.00038113433],"genre_scores_gemma":[0.9993988,0.000058208963,0.00024673413,0.000009232975,0.000002163571,0.000002420939,0.00012229309,0.0000025091401,0.00015773495],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987745,0.0000065635954,0.000009249774,0.00003644087,0.00003233008,0.00003797387],"domain_scores_gemma":[0.99979645,0.000013361913,0.00008549297,0.000013353862,0.000052291412,0.00003906132],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033286028,0.00031474087,0.00018666826,0.0024636784,0.0005718013,0.00040325086,0.000351347,0.0003457367,0.00074110285],"category_scores_gemma":[0.00023697212,0.0002198603,0.00018960367,0.0014457508,0.0006516215,0.00027683488,0.0005038946,0.00011932314,0.00007991605],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000086471686,0.000015974554,0.8492123,0.00008269635,0.0000929617,0.00052368233,0.0015560779,0.00034096034,0.14043158,0.00016590366,0.00009056409,0.0074008307],"study_design_scores_gemma":[0.0000023288194,0.000019098932,0.997673,0.0000026919597,0.000017848044,0.00012837915,0.00031397914,0.00025150282,0.0013568116,0.000017831388,0.00021213105,0.0000043515092],"about_ca_topic_score_codex":0.049055785,"about_ca_topic_score_gemma":0.118016325,"teacher_disagreement_score":0.049055785,"about_ca_system_score_codex":0.00055411115,"about_ca_system_score_gemma":0.0005504232,"threshold_uncertainty_score":0.0975405},"labels":[],"label_agreement":null},{"id":"W4362633234","doi":"10.1029/2022jb025625","title":"Multichannel Sparse Deconvolution of Teleseismic Receiver Functions With <i>f</i> − <i>x</i> Preconditioning","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Deconvolution; Blind deconvolution; Computer science; Robustness (evolution); Algorithm; Noise (video); Compressed sensing; Artificial intelligence; Chemistry; Image (mathematics)","score_opus":0.044210092314512235,"score_gpt":0.3024790598489256,"score_spread":0.25826896753441336,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4362633234","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.053108465,0.0000748012,0.94517577,0.00007182457,0.000030939005,0.000026077194,0.000070835355,0.0003690932,0.0010720625],"genre_scores_gemma":[0.36037418,0.00012464021,0.63638514,0.00005778613,0.000037771144,0.00006407447,0.00026219996,0.00009539987,0.002598789],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997279,0.00006202408,0.000016373764,0.000061464925,0.000094107236,0.000038171176],"domain_scores_gemma":[0.9995894,0.00013410377,0.00007526889,0.00008079841,0.000102891856,0.000017615654],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006333789,0.00068864645,0.00041695012,0.0003443814,0.00022334693,0.00041984738,0.00047717022,0.0005423126,0.0014019427],"category_scores_gemma":[0.0014080234,0.00022968929,0.0005332014,0.0005303892,0.00043517048,0.00065213407,0.0005723308,0.0005376601,0.0004116444],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00052342203,0.00021391442,0.0032033564,0.00020481352,0.00013797957,0.00023458191,0.00018276657,0.46620217,0.15189286,0.019771662,0.0025287261,0.35490373],"study_design_scores_gemma":[0.000011956249,0.000048047314,0.00040877814,0.0000048742104,0.000008921487,0.00005301065,0.000011645761,0.9751101,0.02192303,0.0012404298,0.0011679885,0.00001133049],"about_ca_topic_score_codex":0.004178044,"about_ca_topic_score_gemma":0.0058668484,"teacher_disagreement_score":0.004178044,"about_ca_system_score_codex":0.00033524592,"about_ca_system_score_gemma":0.0011066772,"threshold_uncertainty_score":0.008307457},"labels":[],"label_agreement":null},{"id":"W4366775025","doi":"10.1029/2022jb025505","title":"Water Table and Permeability Estimation From Multi‐Channel Seismoelectric Spectral Ratios","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"Government of Jiangxi Province; National Natural Science Foundation of China","keywords":"Hydrogeology; Vadose zone; Water table; Permeability (electromagnetism); Geology; Relative permeability; Porous medium; Saturation (graph theory); Porosity; Ground truth; Soil science; Mineralogy; Groundwater; Geotechnical engineering; Artificial intelligence; Computer science; Chemistry; Mathematics","score_opus":0.05612998193717426,"score_gpt":0.34011291228624757,"score_spread":0.2839829303490733,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4366775025","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.78411245,0.00020568335,0.21302135,0.00007049682,0.000028283335,0.000027677917,0.00033838878,0.0007199939,0.0014757334],"genre_scores_gemma":[0.9796505,0.00007458276,0.01980365,0.00000892983,0.000007843097,0.000008007741,0.00012955775,0.000016938458,0.00029997117],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999049,0.00001657255,0.00000617596,0.000029884495,0.00002701606,0.000015359208],"domain_scores_gemma":[0.99983525,0.000056475546,0.000037359965,0.0000138737305,0.000043648244,0.000013452628],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023825144,0.0005155047,0.0002633194,0.0011693955,0.00009195793,0.00034726865,0.00030879906,0.0003975527,0.00072841544],"category_scores_gemma":[0.0007515169,0.00020800602,0.00023769532,0.00050471106,0.00020812723,0.00081304734,0.00038766253,0.0002194632,0.00015853414],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005337357,0.00021188386,0.04198065,0.0002706087,0.00013862856,0.00044535572,0.00012671882,0.24892859,0.49177712,0.0012030277,0.0006399993,0.2137437],"study_design_scores_gemma":[0.000014438264,0.00004310087,0.015700758,0.000008480042,0.000021389918,0.00008307435,0.000036085527,0.9426253,0.040586017,0.00057476544,0.0002834486,0.000023090064],"about_ca_topic_score_codex":0.0013125513,"about_ca_topic_score_gemma":0.0015128108,"teacher_disagreement_score":0.0013125513,"about_ca_system_score_codex":0.00012688371,"about_ca_system_score_gemma":0.00015709826,"threshold_uncertainty_score":0.002609849},"labels":[],"label_agreement":null},{"id":"W4367317438","doi":"10.1029/2022jb025912","title":"Viscoelastic Response of a Self‐Gravitational Spherical Earth to Shear Dislocation Obtained Using the Fixed‐Talbot Method","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"China Scholarship Council; National Natural Science Foundation of China","keywords":"Viscoelasticity; Laplace transform; Gravitation; Mechanics; Physics; Classical mechanics; Geometry; Geology; Mathematical analysis; Mathematics","score_opus":0.0669513335210434,"score_gpt":0.3846918266381111,"score_spread":0.31774049311706765,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4367317438","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6513509,0.00014447322,0.3410769,0.0001906759,0.00005580817,0.000032919914,0.00007104506,0.00031236405,0.0067648464],"genre_scores_gemma":[0.97537506,0.00007130294,0.022713881,0.00003354831,0.0000051787515,0.000013157355,0.000040607047,0.00003983687,0.0017071923],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999521,0.000013434659,0.0000023046282,0.0000062539084,0.000016468857,0.000009457098],"domain_scores_gemma":[0.999846,0.000060640818,0.000022408729,0.000018365152,0.00004188454,0.000010753179],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025329835,0.00038827502,0.00021335005,0.00041714916,0.0001622324,0.00042370922,0.00044690864,0.00055649446,0.0009998755],"category_scores_gemma":[0.00066906126,0.00010726812,0.0003618026,0.00032669512,0.00044148602,0.00040016565,0.0003565936,0.00034575124,0.00014362027],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011214992,0.0000979849,0.0037309134,0.000091415015,0.00005160773,0.00048338782,0.0003264617,0.8381063,0.08069302,0.039391056,0.00065513555,0.03626066],"study_design_scores_gemma":[0.0000037101413,0.000013076048,0.00034286754,0.0000031303543,0.0000028543602,0.000016471138,0.000015284155,0.9967854,0.001989857,0.00067668495,0.00014489495,0.000005825027],"about_ca_topic_score_codex":0.00337479,"about_ca_topic_score_gemma":0.0024271682,"teacher_disagreement_score":0.00337479,"about_ca_system_score_codex":0.00036930313,"about_ca_system_score_gemma":0.0003688844,"threshold_uncertainty_score":0.006710291},"labels":[],"label_agreement":null},{"id":"W4377138787","doi":"10.1029/2023jb026602","title":"Seismic Evidence for Metamorphic Densification of the Lower Continental Crust in Eastern North America","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Crust; Craton; Receiver function; Isostasy; Continental crust; Seismology; Metamorphic rock; Tectonics; Mafic; Magma; Petrology; Paleontology; Geochemistry; Lithosphere; Volcano","score_opus":0.10302278066008794,"score_gpt":0.3386499303035283,"score_spread":0.23562714964344036,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4377138787","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984162,0.00008885043,0.00015745847,0.000029590454,7.8341077e-7,0.0000024958745,0.00011093675,0.000028075028,0.0011655184],"genre_scores_gemma":[0.9995782,0.000038868944,0.00013686201,0.000003909507,4.456831e-7,9.282121e-7,0.00010046258,0.0000037473324,0.00013656606],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998772,0.0000136305325,0.000009108877,0.000034675846,0.000039356262,0.000026054435],"domain_scores_gemma":[0.99977535,0.000027571037,0.00006565721,0.00002325468,0.00007361847,0.000034449833],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020370784,0.00025160387,0.00017353355,0.00112861,0.00027213513,0.00085077964,0.0003743157,0.00027734763,0.0013410788],"category_scores_gemma":[0.0005886567,0.00029498074,0.00022425786,0.00095950684,0.0005295239,0.0002776969,0.0006433961,0.00019718558,0.00011562922],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007783754,0.000014909844,0.9634884,0.000040964573,0.000097311415,0.0002234263,0.0005899999,0.009025048,0.015675228,0.00032815302,0.00016617398,0.010272485],"study_design_scores_gemma":[0.000003622614,0.000006319554,0.9954869,0.000007904213,0.000010216528,0.000036271445,0.00023815506,0.003621528,0.00023507875,0.000035822864,0.00031286178,0.0000052064697],"about_ca_topic_score_codex":0.43469632,"about_ca_topic_score_gemma":0.5772921,"teacher_disagreement_score":0.43469632,"about_ca_system_score_codex":0.0017727705,"about_ca_system_score_gemma":0.00078006566,"threshold_uncertainty_score":0.8643322},"labels":[],"label_agreement":null},{"id":"W4379985518","doi":"10.1029/2022jb025817","title":"A Mixed‐Flux‐Based Nodal Discontinuous Galerkin Method for 3D Dynamic Rupture Modeling","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Fault (geology); Discontinuous Galerkin method; Benchmark (surveying); Earthquake rupture; Boundary (topology); Computer science; Geometry; Mechanics; Geology; Mathematical analysis; Mathematics; Physics; Structural engineering; Engineering; Finite element method; Seismology","score_opus":0.07994624622892851,"score_gpt":0.3713197780327263,"score_spread":0.29137353180379777,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4379985518","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.029583607,0.00013924943,0.9679615,0.00008864622,0.00003377871,0.000042973305,0.00007034946,0.00028108808,0.0017987997],"genre_scores_gemma":[0.66199523,0.00021536944,0.33414665,0.00007670121,0.000035730896,0.00027757307,0.00017494122,0.00017087047,0.0029068221],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998622,0.00004967949,0.00000824217,0.000018888064,0.000048057424,0.000012975598],"domain_scores_gemma":[0.9997131,0.00014769529,0.0000318245,0.00001924827,0.00006544733,0.000022606842],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00048949564,0.00059839356,0.00064619863,0.0005685637,0.0003747631,0.00067461823,0.0011572052,0.0010258538,0.0016936533],"category_scores_gemma":[0.00080770906,0.00043418803,0.00065212813,0.0003467539,0.0006041552,0.0005652487,0.0006666439,0.00072987675,0.00028207386],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003125546,0.000041933457,0.00058243447,0.000046045367,0.000022291772,0.000053909807,0.00004470277,0.9773842,0.0042325007,0.0045103943,0.00022242877,0.012827992],"study_design_scores_gemma":[0.0000015990017,0.000002763362,0.000014301593,9.673136e-7,7.5650365e-7,0.0000015655386,0.0000011684698,0.9996113,0.00012560587,0.00014299405,0.000096021715,0.0000011105969],"about_ca_topic_score_codex":0.0048210295,"about_ca_topic_score_gemma":0.0034669817,"teacher_disagreement_score":0.0048210295,"about_ca_system_score_codex":0.00053669745,"about_ca_system_score_gemma":0.0008211476,"threshold_uncertainty_score":0.009585917},"labels":[],"label_agreement":null},{"id":"W4380791981","doi":"10.1029/2022jb025486","title":"Focusing Effects of Teleseismic Wavefields by the Subducting Plate Beneath Cascadia","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Subduction; Seismology; Amplitude; Slab; Attenuation; Azimuth; Seismic wave; Broadband; Scattering; Geophysics; Tectonics; Physics; Optics","score_opus":0.029665225663815152,"score_gpt":0.3092431899630287,"score_spread":0.27957796429921355,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4380791981","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992157,0.000008080053,0.00021268937,0.0000122831025,5.7410057e-7,0.0000013684162,0.00003896822,0.00002583751,0.00048439144],"genre_scores_gemma":[0.9997559,0.000010416371,0.00012327335,0.0000013323307,5.095584e-7,9.4649636e-7,0.00002926999,0.0000025239228,0.00007581516],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993145,0.000009632963,0.0000041201147,0.000018739229,0.000021475598,0.000014538032],"domain_scores_gemma":[0.999856,0.000037537815,0.000035404293,0.000015511869,0.00003416387,0.000021330772],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011754591,0.00046498692,0.00015073648,0.00053111464,0.00028034564,0.00031552053,0.00029022974,0.0002009664,0.0006757453],"category_scores_gemma":[0.0005735218,0.00027273982,0.00019811354,0.0004283673,0.00032796178,0.00015842097,0.00037523624,0.00014534761,0.000094667674],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003887096,0.00012894778,0.63029724,0.00006290846,0.00015304108,0.00066887814,0.00068790343,0.19789599,0.14929456,0.00061828556,0.0003530567,0.019450508],"study_design_scores_gemma":[0.000037753904,0.000083424275,0.81881756,0.0000113707065,0.000056486784,0.00009927951,0.0002612361,0.17207094,0.007921861,0.00024460925,0.00037275345,0.000022785101],"about_ca_topic_score_codex":0.08678545,"about_ca_topic_score_gemma":0.07144917,"teacher_disagreement_score":0.08678545,"about_ca_system_score_codex":0.0010529206,"about_ca_system_score_gemma":0.0004743912,"threshold_uncertainty_score":0.17256057},"labels":[],"label_agreement":null},{"id":"W4381125304","doi":"10.1029/2023jb026555","title":"Magnetotelluric Imaging of the Lithospheric Structure of the Southern Oklahoma Aulacogen: Evidence for Long‐Term Weakening Caused by Rifting","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Lithosphere; Geology; Lithospheric flexure; Mantle (geology); Orogeny; Asthenosphere; Rift; Geophysics; Crust; Mantle plume; Petrology; Seismology; Tectonics","score_opus":0.04079565183821265,"score_gpt":0.3081582698443711,"score_spread":0.26736261800615846,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4381125304","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992393,0.00003978051,0.00003711652,0.000019283618,9.0325483e-7,0.000001601362,0.00019299248,0.0000065250415,0.00046242063],"genre_scores_gemma":[0.9995845,0.000023700537,0.00009745089,0.000008283822,0.00000175864,0.0000017031691,0.00014074784,0.0000013826082,0.00014053432],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999577,0.0000028354302,0.0000022415772,0.000010161516,0.000009418736,0.000017678633],"domain_scores_gemma":[0.99984443,0.0000168165,0.00004453153,0.00001234588,0.000049774113,0.00003201557],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000083002815,0.00013569095,0.000112683854,0.00066412,0.00049704505,0.0004293482,0.00017085372,0.00021579649,0.0007781416],"category_scores_gemma":[0.00021467435,0.00010877673,0.00005858322,0.00080881355,0.00018176214,0.00016136783,0.00023840119,0.00016055806,0.000118633805],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001506723,0.000037259204,0.8799315,0.000046253408,0.00005705251,0.00042505073,0.00075241766,0.0005993464,0.10630291,0.000071455404,0.00032042328,0.011305613],"study_design_scores_gemma":[0.0000023277898,0.0000070716696,0.9982595,0.000003367429,0.000008122732,0.00002570288,0.00021469122,0.0003239046,0.000846574,0.000005501013,0.00030093433,0.0000023037617],"about_ca_topic_score_codex":0.0982049,"about_ca_topic_score_gemma":0.21055622,"teacher_disagreement_score":0.0982049,"about_ca_system_score_codex":0.00075998734,"about_ca_system_score_gemma":0.00037670034,"threshold_uncertainty_score":0.1952666},"labels":[],"label_agreement":null},{"id":"W4383550556","doi":"10.1029/2023jb026890","title":"Thank You to Our 2022 Peer Reviewers","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Academic Publishing and Open Access","field":"Decision Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Syracuse University","keywords":"Peer review; Psychology; Library science; Political science; Computer science; Law","score_opus":0.2651838731009451,"score_gpt":0.5479478971805788,"score_spread":0.2827640240796337,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4383550556","genre_codex":"editorial","genre_gemma":"editorial","domain_codex":null,"domain_gemma":"evaluation","model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"editorial","genre_consensus":"editorial","domain_candidate":"evaluation","domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0012458793,0.00991044,0.0056511085,0.28475016,0.6682537,0.0006037937,0.0028243281,0.0035987955,0.023161868],"genre_scores_gemma":[0.014360396,0.011150624,0.01617886,0.15288731,0.3396823,0.0013514842,0.0044081933,0.0070378203,0.45294303],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9775932,0.0046977475,0.0020221174,0.0029939476,0.011629523,0.001063395],"domain_scores_gemma":[0.5536757,0.012672996,0.011038747,0.010266213,0.38656348,0.02578293],"candidate_categories":["metaresearch"],"consensus_categories":[],"category_scores_codex":[0.016081968,0.0017907122,0.0023530729,0.0039608423,0.004539074,0.014645945,0.0025829868,0.004854118,0.13680594],"category_scores_gemma":[0.18653385,0.0009175923,0.0014451892,0.0025739816,0.0018703439,0.006743322,0.004756963,0.0073857596,0.21545097],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016179996,0.0000050978742,0.00015646062,0.000058523918,0.0000053834015,0.0000638151,0.000060081362,0.000014939054,0.00011217582,0.00015544941,0.9878226,0.011529337],"study_design_scores_gemma":[0.000011919937,0.000008975889,0.00034639638,0.00008661999,0.000010648056,0.00016909516,0.0002951548,0.00006616818,0.00013022014,0.0005541557,0.9982899,0.00003075601],"about_ca_topic_score_codex":0.0045648334,"about_ca_topic_score_gemma":0.011461426,"teacher_disagreement_score":0.983918,"about_ca_system_score_codex":0.0019462096,"about_ca_system_score_gemma":0.009092999,"threshold_uncertainty_score":0.45766145},"labels":[],"label_agreement":null},{"id":"W4386998048","doi":"10.1029/2023jb027274","title":"Modes of Mantle Convection, Their Stability, and What Controls Their Existence","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa; Geological Survey of Canada; Natural Resources Canada","funders":"David and Lucile Packard Foundation","keywords":"Mantle convection; Convection; Mantle (geology); Rayleigh number; Geophysics; Geology; Plate tectonics; Physics; Mechanics; Natural convection; Tectonics; Lithosphere","score_opus":0.07012139041216651,"score_gpt":0.31869705933074505,"score_spread":0.24857566891857852,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386998048","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9664596,0.0007838896,0.019073695,0.000494558,0.000039502975,0.0000142350345,0.00008159169,0.00009595723,0.012957007],"genre_scores_gemma":[0.99880576,0.00007745505,0.0007379836,0.000011188124,0.000013511615,0.000007597182,0.000013580082,0.000010634191,0.0003222733],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997975,0.000039951654,0.0000117145655,0.00006960487,0.000037061676,0.00004423557],"domain_scores_gemma":[0.9989386,0.0003293909,0.00031432047,0.00010787594,0.00014241795,0.0001673499],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005956054,0.00021278507,0.00024873804,0.00081656297,0.00059031753,0.0015807737,0.00045745654,0.0003224325,0.0018076478],"category_scores_gemma":[0.0039299363,0.00015821324,0.0001988592,0.0002588681,0.0018290272,0.001438182,0.000811514,0.00046528806,0.000230753],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005307746,0.00010442745,0.1864663,0.00028199336,0.00014166717,0.00033689407,0.004208721,0.058715984,0.11344602,0.55334425,0.0039026374,0.07852043],"study_design_scores_gemma":[0.00007509596,0.00014819084,0.19222066,0.00016353888,0.00006443999,0.00036202947,0.002848336,0.31357107,0.013853069,0.4694136,0.007073482,0.00020649548],"about_ca_topic_score_codex":0.0025423407,"about_ca_topic_score_gemma":0.0013292257,"teacher_disagreement_score":0.0025423407,"about_ca_system_score_codex":0.00067735754,"about_ca_system_score_gemma":0.00031686013,"threshold_uncertainty_score":0.006047249},"labels":[],"label_agreement":null},{"id":"W4387078932","doi":"10.1029/2023jb027428","title":"Variations of Crustal Thickness in Alaska and Northwestern Canada: Implications for Crustal Modification and Accretion of Tectonic Units","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Terrane; Subduction; Seismology; Tectonics; Accretion (finance); Craton; Crust; Continental margin; North American Plate; Plate tectonics; Continental crust; Paleontology","score_opus":0.058418629863625886,"score_gpt":0.32459378735528743,"score_spread":0.26617515749166154,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387078932","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986268,0.00010084198,0.000054170054,0.000015658092,0.000001300785,0.0000014760644,0.00036276158,0.0000046824844,0.00083238014],"genre_scores_gemma":[0.999308,0.000059388836,0.000075634984,0.0000034965958,5.973174e-7,9.2243954e-7,0.0002538155,0.0000012541815,0.00029686574],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991906,0.00000459743,0.000004768385,0.000020324002,0.000022081027,0.000029176548],"domain_scores_gemma":[0.9996412,0.000029970703,0.00007065138,0.000013738479,0.00016107445,0.00008333504],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015761786,0.00022581388,0.00013774628,0.0010918742,0.0007741687,0.0007055508,0.00022642832,0.00016252272,0.0010723936],"category_scores_gemma":[0.0005913585,0.000102601334,0.00014877874,0.0013164105,0.000308621,0.00020242261,0.0003894839,0.00013594635,0.00009407912],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004658664,0.000007814754,0.99133426,0.000007319569,0.00002803192,0.00008694172,0.00028855147,0.0008988018,0.003176933,0.00007396085,0.0000938732,0.003956931],"study_design_scores_gemma":[7.238334e-7,0.0000018623587,0.99881124,0.0000037569587,0.0000055472333,0.000016155465,0.0003803729,0.00049124163,0.00015121159,0.000011815963,0.00012368405,0.0000023263237],"about_ca_topic_score_codex":0.8989696,"about_ca_topic_score_gemma":0.9391468,"teacher_disagreement_score":0.10103041,"about_ca_system_score_codex":0.0031371359,"about_ca_system_score_gemma":0.0022182232,"threshold_uncertainty_score":0.20325077},"labels":[],"label_agreement":null},{"id":"W4388464397","doi":"10.1029/2023jb026482","title":"Long‐Lived Aftershocks in the New Madrid seismic Zone and the Rest of Stable North America","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Aftershock; Induced seismicity; Seismology; Geology; Seismic hazard; Magnitude (astronomy)","score_opus":0.04202204991743295,"score_gpt":0.3038474530686018,"score_spread":0.2618254031511688,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388464397","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989287,0.00012320565,0.000047172092,0.000024038205,0.0000035312462,0.0000025666902,0.00014539315,0.00000254515,0.0007227855],"genre_scores_gemma":[0.99938476,0.00006232673,0.00005278665,0.000008178177,0.000004643142,0.0000021180365,0.0003128462,0.0000013259519,0.00017099353],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998267,0.000029385454,0.000012119004,0.000048211055,0.000038409795,0.000045222165],"domain_scores_gemma":[0.9990214,0.00015824345,0.0003475145,0.000046605954,0.00022588605,0.00020031758],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002955976,0.0001290086,0.00018371308,0.0011759872,0.00033490348,0.00046093113,0.00023414363,0.00016482009,0.0010057617],"category_scores_gemma":[0.0013140792,0.00006295514,0.00015721185,0.0010439577,0.0003143031,0.00031588468,0.00048078876,0.00018476238,0.00013241495],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006934511,0.000017234419,0.99517584,0.000013544698,0.00004761858,0.00008339058,0.00039154125,0.00025010362,0.00049097766,0.000087286375,0.00028258568,0.0030905053],"study_design_scores_gemma":[0.0000015209599,0.0000049157343,0.9990381,0.000003689884,0.000005790825,0.000012977755,0.0004789977,0.00020982923,0.000030094465,0.00001607164,0.00019652507,0.0000015802334],"about_ca_topic_score_codex":0.1324364,"about_ca_topic_score_gemma":0.20578818,"teacher_disagreement_score":0.8675636,"about_ca_system_score_codex":0.0007441701,"about_ca_system_score_gemma":0.00038624232,"threshold_uncertainty_score":0.26333106},"labels":[],"label_agreement":null},{"id":"W4388871450","doi":"10.1029/2023jb026806","title":"Modeling Multi‐Material Structural Patterns in Tectonic Flow With a Discontinuous Galerkin Level Set Method","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Enhanced Oil Recovery Techniques","field":"Engineering","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Finite element method; Geology; Flow (mathematics); Discontinuous Galerkin method; Geometry; Computer science; Mechanics; Computational science; Mathematics; Physics; Structural engineering; Engineering","score_opus":0.0757384787921097,"score_gpt":0.3830840265414321,"score_spread":0.3073455477493224,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388871450","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.06410016,0.00008600229,0.93290013,0.0001516058,0.000030402061,0.00004685318,0.000066657616,0.0002255594,0.0023926646],"genre_scores_gemma":[0.7823428,0.00013287527,0.21424632,0.00008212669,0.000024602577,0.00019316391,0.00011897011,0.000097492986,0.0027617323],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997925,0.00007470851,0.00001026649,0.000023535667,0.00007855936,0.00002040731],"domain_scores_gemma":[0.99961084,0.000238536,0.000044289143,0.000029538009,0.000053048887,0.000023762315],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00054155744,0.0005350359,0.00053230516,0.0008292901,0.00039173767,0.001032495,0.0009609931,0.0012694799,0.00096199353],"category_scores_gemma":[0.0010263324,0.00048699338,0.00073969946,0.00041482,0.001144614,0.00054578803,0.0006795524,0.0008847805,0.00019838651],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000054473107,0.000015631214,0.00025680775,0.000007770053,0.000004735166,0.000017771197,0.000018670184,0.9933907,0.0013340932,0.002679553,0.00005065731,0.0022181992],"study_design_scores_gemma":[0.0000011058983,0.0000020077455,0.00002230035,7.9986455e-7,4.8012544e-7,0.000001483091,0.000001104111,0.99947065,0.00013526059,0.0003033196,0.000060355764,0.0000011494884],"about_ca_topic_score_codex":0.005158835,"about_ca_topic_score_gemma":0.0030921884,"teacher_disagreement_score":0.005158835,"about_ca_system_score_codex":0.000861801,"about_ca_system_score_gemma":0.00096452143,"threshold_uncertainty_score":0.010257602},"labels":[],"label_agreement":null},{"id":"W4388991842","doi":"10.1029/2023jb026789","title":"Osmium Isotope Heterogeneity of the Upper Mantle: Evidence From the Bay of Islands Ophiolite Complex, Newfoundland","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"National Key Research and Development Program of China; China University of Geosciences, Beijing; National Natural Science Foundation of China","keywords":"Ophiolite; Geology; Mantle (geology); Geochemistry; Partial melting; Peridotite; Subduction; Radiogenic nuclide; Mantle wedge; Basalt; Paleontology; Tectonics","score_opus":0.08574676668402889,"score_gpt":0.33061791695895676,"score_spread":0.24487115027492787,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388991842","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99876714,0.00010111927,0.00003520976,0.000015071506,6.522658e-7,0.0000018811743,0.0002196178,0.0000045735665,0.0008548163],"genre_scores_gemma":[0.99935454,0.00007593708,0.00007451529,0.000008238149,7.1302617e-7,0.0000014460395,0.00021798344,0.0000027059205,0.00026401566],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986744,0.0000071397717,0.000008442396,0.000035161964,0.000028428842,0.000053344203],"domain_scores_gemma":[0.9997851,0.00002153262,0.000063011044,0.000014040128,0.00008100552,0.000035215442],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015323125,0.00021132406,0.00018229186,0.0020251868,0.00076153333,0.0007884954,0.00034749435,0.00015068433,0.0011651325],"category_scores_gemma":[0.00030777094,0.00017734917,0.00011979672,0.0014428337,0.00072185544,0.000223146,0.0005436676,0.00014231713,0.00011660069],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013454419,0.000013094511,0.9513656,0.000049240716,0.00007876821,0.00034237694,0.0014327215,0.00016760286,0.039163884,0.00011035916,0.00019411037,0.0069476613],"study_design_scores_gemma":[0.000001811303,0.00000617857,0.99821365,0.0000043741147,0.000010938035,0.000051708263,0.00047250575,0.000079591875,0.0007261517,0.0000059884123,0.0004251163,0.0000019424792],"about_ca_topic_score_codex":0.7158348,"about_ca_topic_score_gemma":0.87862414,"teacher_disagreement_score":0.2841652,"about_ca_system_score_codex":0.002970589,"about_ca_system_score_gemma":0.0010636197,"threshold_uncertainty_score":0.5716774},"labels":[],"label_agreement":null},{"id":"W4389206890","doi":"10.1029/2023jb027349","title":"On the Potential Role of Viscoelasticity in Fluid‐Induced Seismicity","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Hotchkiss Brain Institute; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Alberta Innovates; Microseismic Industry Consortium","keywords":"Aftershock; Induced seismicity; Geology; Viscoelasticity; Geothermal gradient; Seismology; Geomechanics; Hydraulic fracturing; Rheology; Tectonics; Fluid dynamics; Geotechnical engineering; Geophysics; Mechanics; Physics","score_opus":0.04427291331815409,"score_gpt":0.3141495109711545,"score_spread":0.2698765976530004,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389206890","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9399028,0.00029238354,0.05638071,0.00034057593,0.000032042804,0.000026985037,0.000080491714,0.00015444927,0.0027896147],"genre_scores_gemma":[0.99889225,0.00007655988,0.00080782,0.000008595755,0.0000044912795,0.0000041340504,0.000010073156,0.000005327355,0.0001906176],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991775,0.00002342959,0.000004835264,0.000020507068,0.000012931178,0.000020598325],"domain_scores_gemma":[0.9991431,0.00048806408,0.00017968936,0.000060552436,0.000051596737,0.00007688726],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025066597,0.0004480665,0.00030622643,0.00042609434,0.00025618906,0.00073212996,0.00053424074,0.0008180248,0.0011230807],"category_scores_gemma":[0.0016315224,0.00023247195,0.00034963037,0.00022270136,0.00090785493,0.000992502,0.0005701263,0.00040472197,0.00007855287],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010265851,0.00014600933,0.008337296,0.000076476535,0.00003711399,0.00035470002,0.00007581745,0.93026656,0.04817137,0.00779929,0.0001397741,0.0044929394],"study_design_scores_gemma":[0.0000044639223,0.000029561208,0.0013802408,0.0000037463553,0.0000074421237,0.00001891892,0.000010936001,0.99525166,0.0019131046,0.0013011765,0.000071234805,0.0000074684017],"about_ca_topic_score_codex":0.0027273253,"about_ca_topic_score_gemma":0.001135787,"teacher_disagreement_score":0.0027273253,"about_ca_system_score_codex":0.00031570796,"about_ca_system_score_gemma":0.00028039457,"threshold_uncertainty_score":0.00542289},"labels":[],"label_agreement":null},{"id":"W4389606669","doi":"10.1029/2023jb026793","title":"New Insights Into the Active Tectonics of the Northern Canadian Cordillera From an Enhanced Earthquake Catalog","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Colorado State University; National Science Foundation","keywords":"Geology; Seismology; Induced seismicity; Foreland basin; Crust; Tectonics; Active fault; Thrust fault; Fault (geology); Structural basin; Paleontology","score_opus":0.030382970479641443,"score_gpt":0.29878563229250227,"score_spread":0.2684026618128608,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389606669","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.978573,0.00063088053,0.0007846966,0.00018899453,0.000006103948,0.0000323177,0.012361758,0.00008036373,0.0073418836],"genre_scores_gemma":[0.98256665,0.00043850468,0.0023685023,0.000028947576,0.000010652742,0.000015820975,0.011891057,0.000016206852,0.002663704],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990416,0.000005037261,0.0000058935034,0.000026518655,0.000029981931,0.000028351584],"domain_scores_gemma":[0.9995906,0.000033274984,0.00006679161,0.000033819684,0.00020496106,0.00007047722],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016379938,0.00031941364,0.00016504577,0.003891877,0.00071078446,0.0008642965,0.00027893024,0.00014466664,0.0026849054],"category_scores_gemma":[0.00080867746,0.00009979538,0.00014487357,0.0047571817,0.0002015294,0.00020481776,0.00051064277,0.00013838189,0.00024138049],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008677376,0.000035369336,0.8754064,0.00008153367,0.00007542372,0.000358625,0.0010406176,0.0039127073,0.008644248,0.00083291886,0.005363309,0.10416213],"study_design_scores_gemma":[0.0000027446645,0.000003952249,0.99269706,0.000011254088,0.000013102343,0.000035527384,0.0003264322,0.0016558105,0.00018760376,0.00005836938,0.0050027026,0.000005552311],"about_ca_topic_score_codex":0.9517142,"about_ca_topic_score_gemma":0.987456,"teacher_disagreement_score":0.048285782,"about_ca_system_score_codex":0.0034677777,"about_ca_system_score_gemma":0.003369348,"threshold_uncertainty_score":0.09714025},"labels":[],"label_agreement":null},{"id":"W4390014613","doi":"10.1029/2023jb026771","title":"Joint Inversion of SPREE Receiver Functions and Surface Wave Dispersion Curves for 3‐D Crustal and Upper Mantle Structure Beneath the U.S. Midcontinent Rift","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba; Université du Québec à Montréal","funders":"","keywords":"Geology; Rift; Crust; Underplating; Mantle (geology); Seismology; Receiver function; Mafic; Continental crust; Petrology; Geophysics; Tectonics; Lithosphere","score_opus":0.041769417579681355,"score_gpt":0.28480460085322007,"score_spread":0.2430351832735387,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4390014613","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99747616,0.000031234773,0.0015500775,0.00003865965,0.0000028838326,0.0000040549735,0.0004370608,0.000117192925,0.00034277694],"genre_scores_gemma":[0.9967405,0.00001540948,0.0021670852,0.000006462904,0.0000021184203,0.000002788975,0.0007790592,0.000007917473,0.00027859845],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994576,0.000008348195,0.0000024772478,0.000017543558,0.000012132173,0.000013639399],"domain_scores_gemma":[0.99987996,0.000022774113,0.00002134836,0.000014363425,0.000042441505,0.000019093015],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025099167,0.00040292824,0.00013873941,0.0004886872,0.00019195954,0.00040014295,0.00022706132,0.0002552701,0.00052983616],"category_scores_gemma":[0.0005889884,0.00021790998,0.0003653583,0.00030881053,0.000097312484,0.00025512485,0.0002865851,0.00018313926,0.00013642397],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003185838,0.00020360021,0.6073273,0.000047461985,0.00034612924,0.00041219356,0.00068142754,0.20253283,0.09107172,0.00063012855,0.0015183557,0.09491035],"study_design_scores_gemma":[0.000031782565,0.000055813885,0.65685546,0.000010543004,0.00005863279,0.00005425006,0.00021422577,0.3365774,0.00494431,0.00019458805,0.0009786733,0.000024324077],"about_ca_topic_score_codex":0.06920688,"about_ca_topic_score_gemma":0.12613823,"teacher_disagreement_score":0.06920688,"about_ca_system_score_codex":0.0003804967,"about_ca_system_score_gemma":0.00053226936,"threshold_uncertainty_score":0.13760811},"labels":[],"label_agreement":null},{"id":"W4390486996","doi":"10.1029/2023jb027276","title":"Control of Seismicity Migration in Earthquake Swarms by Injected Fluid Volume and Aseismic Crack Propagation","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Agence Nationale de la Recherche","keywords":"Induced seismicity; Geology; Seismic moment; Seismology; Slip (aerodynamics); Fluid dynamics; Fluid pressure; Geothermal gradient; Front (military); Fault (geology); Mechanics; Geophysics; Physics","score_opus":0.01935156711211921,"score_gpt":0.2878030788456735,"score_spread":0.2684515117335543,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4390486996","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99393773,0.00003368319,0.0055637057,0.000018092334,0.0000020064078,0.0000032337973,0.000022598324,0.000028309933,0.00039064372],"genre_scores_gemma":[0.99976045,0.000007467089,0.00017382385,8.0431033e-7,5.286963e-7,0.00000104384,0.0000052289406,0.000001735133,0.000048925296],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99995923,0.000010359658,0.0000030643657,0.000010004145,0.0000069810685,0.0000102674085],"domain_scores_gemma":[0.99965274,0.00013127559,0.0001298883,0.000015525186,0.000028816692,0.000041682608],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012278037,0.00018670171,0.00015135898,0.00037729408,0.000109110726,0.0003713502,0.00021357964,0.00024120428,0.00042425527],"category_scores_gemma":[0.0007602669,0.00014881734,0.00020095835,0.000114167015,0.00041109207,0.00019377441,0.00021446218,0.0001604875,0.000049180235],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031448656,0.00025977675,0.07404132,0.00006762604,0.000102272206,0.00058910693,0.00021183645,0.48080397,0.42644423,0.0041403403,0.00020796385,0.012817106],"study_design_scores_gemma":[0.000016425467,0.00008337405,0.028839247,0.0000035373548,0.000012771042,0.0000519531,0.000038526243,0.9596507,0.010730232,0.0004681718,0.000093184135,0.000011937959],"about_ca_topic_score_codex":0.0033591476,"about_ca_topic_score_gemma":0.0019351052,"teacher_disagreement_score":0.0033591476,"about_ca_system_score_codex":0.00036615122,"about_ca_system_score_gemma":0.00018421213,"threshold_uncertainty_score":0.0066791773},"labels":[],"label_agreement":null},{"id":"W4390650651","doi":"10.1029/2023jb027646","title":"Lithosphere Removal in the Sierra Nevada de Santa Marta, Colombia","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Tectonic Studies in Latin America","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Alliance de recherche numérique du Canada; Compute Canada; Cement Association of Canada; National Science Foundation","keywords":"Lithosphere; Geology; Bouguer anomaly; Mantle (geology); Gravity anomaly; Crust; Lithospheric flexure; Magmatism; Geophysics; Seismology; Tectonics; Paleontology","score_opus":0.04162268661988454,"score_gpt":0.345578581325015,"score_spread":0.30395589470513046,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4390650651","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99573624,0.00031187476,0.00032142474,0.000087283144,0.0000100782845,0.00000728579,0.000381447,0.00005329811,0.003091109],"genre_scores_gemma":[0.9992586,0.00008500896,0.00019182384,0.0000072318685,0.0000014980358,0.0000030090443,0.00015276388,0.0000054689267,0.00029448787],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99993145,0.000009976866,0.0000038872836,0.000018782312,0.000013022986,0.000022798495],"domain_scores_gemma":[0.9998627,0.000033018878,0.0000406927,0.000012874013,0.000027171549,0.000023571709],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000089456924,0.00034362337,0.00028569793,0.0004845241,0.00049632206,0.0009952072,0.0005868085,0.00044686964,0.0013682161],"category_scores_gemma":[0.0006292762,0.00016039985,0.00038226877,0.00034107466,0.0002826993,0.0003022772,0.00036834655,0.00024487753,0.00011207251],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039901663,0.00015374867,0.35242906,0.00030586403,0.00019981744,0.0015390292,0.00044068872,0.6044197,0.016412802,0.0023169483,0.0012657978,0.02011758],"study_design_scores_gemma":[0.00011798633,0.00013096465,0.349409,0.0000591467,0.00010969682,0.0002641575,0.0010887466,0.638786,0.003005905,0.00079842255,0.0061485157,0.00008140478],"about_ca_topic_score_codex":0.3688364,"about_ca_topic_score_gemma":0.33922422,"teacher_disagreement_score":0.3688364,"about_ca_system_score_codex":0.002908929,"about_ca_system_score_gemma":0.0010031019,"threshold_uncertainty_score":0.73337907},"labels":[],"label_agreement":null},{"id":"W4391392571","doi":"10.1029/2023jb027329","title":"Deep Structure of the Santos Basin, Offshore Brazil From 3D Inversion of magnetotelluric Data","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geoscience BC","funders":"","keywords":"Magnetotellurics; Geology; Submarine pipeline; Inversion (geology); Structural basin; Seismology; Paleontology; Oceanography; Engineering","score_opus":0.04099172747107104,"score_gpt":0.33381806287695226,"score_spread":0.2928263354058812,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391392571","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978381,0.00004311753,0.0009992763,0.000055336084,0.000002224377,0.000004458759,0.0003669689,0.00010142941,0.00058907963],"genre_scores_gemma":[0.99896765,0.000019556695,0.00061527523,0.0000039317965,0.0000012066141,0.000002134979,0.00031951597,0.0000066736843,0.00006410553],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993527,0.0000107931,0.000005106075,0.000021998383,0.000013753546,0.000013064635],"domain_scores_gemma":[0.99983406,0.00004088443,0.000037212492,0.000022812674,0.000042982516,0.00002205699],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017163437,0.00034338233,0.00022748127,0.0006384304,0.00019554245,0.00061888207,0.00037586046,0.00032061417,0.0006036317],"category_scores_gemma":[0.0008754135,0.00030612954,0.0003990063,0.0005811373,0.00025552727,0.00025539304,0.00044457483,0.00018346171,0.00013310614],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034117032,0.00019647091,0.59280306,0.00015236154,0.00042093048,0.0009697489,0.001261936,0.28051385,0.06384359,0.0013168375,0.0010454498,0.0571346],"study_design_scores_gemma":[0.0000770338,0.000057285706,0.45694155,0.000044354096,0.00008140908,0.00013084334,0.00051059335,0.5362105,0.0036781484,0.0005379511,0.0016838353,0.000046443925],"about_ca_topic_score_codex":0.0675195,"about_ca_topic_score_gemma":0.09436698,"teacher_disagreement_score":0.0675195,"about_ca_system_score_codex":0.000453319,"about_ca_system_score_gemma":0.0006089328,"threshold_uncertainty_score":0.13425297},"labels":[],"label_agreement":null},{"id":"W4392194003","doi":"10.1029/2023jb028146","title":"On the Unloading‐Induced Fault Reactivation: The Effect of Stress Path on Failure Criterion and Rupture Dynamics","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Rock Mechanics and Modeling","field":"Engineering","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Tianjin University; China Postdoctoral Science Foundation; National Natural Science Foundation of China","keywords":"Fault (geology); Stress (linguistics); Stress path; Geology; Strain gauge; Geotechnical engineering; Structural engineering; Mechanics; Seismology; Engineering; Physics; Petrology; Shear (geology)","score_opus":0.018486041292044623,"score_gpt":0.3051777408862796,"score_spread":0.28669169959423496,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392194003","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982693,0.00014024385,0.001299785,0.000017856755,0.000006343536,0.0000085114725,0.00004380439,0.000021660811,0.00019256184],"genre_scores_gemma":[0.99939764,0.00006302676,0.0003951131,0.000009225861,0.0000021337319,0.0000072114067,0.000031781852,0.0000052636647,0.0000886119],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998022,0.00002361535,0.000019738629,0.00004658605,0.0000576803,0.000050229733],"domain_scores_gemma":[0.9992933,0.00030752463,0.00015192738,0.00009639591,0.000089014175,0.00006190095],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029922868,0.0003104879,0.00031455432,0.00026112905,0.00019552586,0.00030702888,0.00031676833,0.00029911514,0.0020238275],"category_scores_gemma":[0.00079969293,0.00014082964,0.00016075368,0.00014164766,0.000504725,0.00038148713,0.00031622217,0.00037652534,0.0001685595],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027393285,0.00009347914,0.0031089573,0.000082109815,0.000007843418,0.00020070333,0.000077109,0.0026047358,0.9872312,0.000059244903,0.000050850875,0.0062098727],"study_design_scores_gemma":[0.00002621871,0.0014210244,0.06772703,0.000019142106,0.000019986492,0.00020857787,0.00022942602,0.03227895,0.89729804,0.00018032655,0.00055235863,0.000038947393],"about_ca_topic_score_codex":0.0004314795,"about_ca_topic_score_gemma":0.0006427673,"teacher_disagreement_score":0.0020238275,"about_ca_system_score_codex":0.00018362027,"about_ca_system_score_gemma":0.00013227032,"threshold_uncertainty_score":0.006770313},"labels":[],"label_agreement":null},{"id":"W4392348214","doi":"10.1029/2023jb028463","title":"The Timescale and Carbon Flux Recorded by Skarn Garnet From Gangdese Arc, Southern Tibet","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Skarn; Flux (metallurgy); Geology; Arc (geometry); Geochemistry; Carbon fibers; Carbon flux; Earth science; Materials science; Metallurgy; Seismology; Fluid inclusions; Geometry","score_opus":0.01836135322277706,"score_gpt":0.26885127552180993,"score_spread":0.2504899222990329,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392348214","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99909043,0.00004331818,0.000018204088,0.000008685624,0.000001137057,0.0000011387193,0.00038979444,0.0000047357134,0.00044248955],"genre_scores_gemma":[0.99899405,0.00004262361,0.000041385014,0.0000048109546,0.000003122045,0.000002231546,0.00065541087,0.0000024423855,0.00025393354],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994767,0.0000046240407,0.0000050463514,0.000016085183,0.000010806417,0.000015722315],"domain_scores_gemma":[0.999882,0.000013901544,0.00003515523,0.0000071189206,0.000031948723,0.00002986757],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012852837,0.00027936537,0.00015334583,0.002618224,0.0006089572,0.00044587633,0.00025893893,0.00023669258,0.0012260351],"category_scores_gemma":[0.00018272482,0.00012076809,0.00014766333,0.0020253353,0.00034145694,0.00023605837,0.0003763653,0.00012732865,0.00020456385],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014096462,0.000023870543,0.9697463,0.000064618296,0.00005290429,0.0006008249,0.0014334735,0.0005968806,0.01865195,0.00009945529,0.00024197028,0.008346802],"study_design_scores_gemma":[0.0000021134283,0.000009261012,0.9987387,0.0000056368726,0.0000065995046,0.000068360605,0.0003497568,0.00026180042,0.00022920796,0.000012999045,0.00031356094,0.0000020350747],"about_ca_topic_score_codex":0.048598,"about_ca_topic_score_gemma":0.10916291,"teacher_disagreement_score":0.048598,"about_ca_system_score_codex":0.0005961765,"about_ca_system_score_gemma":0.00026108252,"threshold_uncertainty_score":0.096630216},"labels":[],"label_agreement":null},{"id":"W4392590579","doi":"10.1029/2023jb028307","title":"A New Negative Carbon Isotope Interval Caused by Manganese Redox Cycling After the Shuram Excursion","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Radioactive element chemistry and processing","field":"Chemistry","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"China Scholarship Council; National Natural Science Foundation of China","keywords":"Excursion; Manganese; Redox; Cycling; Carbon fibers; Isotopes of carbon; Chemistry; Isotope; Environmental chemistry; Materials science; Inorganic chemistry; Physics; Total organic carbon; History; Political science","score_opus":0.024444948476023135,"score_gpt":0.34934589136563887,"score_spread":0.32490094288961574,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392590579","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99805415,0.00012374221,0.0004665515,0.00004472837,0.000015845846,0.0000053941167,0.00009666481,0.000047903915,0.0011450637],"genre_scores_gemma":[0.9992804,0.000024300047,0.00021952477,0.00002616292,0.000010081588,0.0000032920832,0.00010459351,0.00000741024,0.00032424758],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99993753,0.0000033127885,0.0000035509695,0.000023663773,0.00001774229,0.000014115308],"domain_scores_gemma":[0.99978656,0.000022342443,0.00005910999,0.000021753522,0.000073334864,0.000036985217],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018549935,0.00022395828,0.00025187962,0.0006779271,0.0003255522,0.00028752518,0.00035135218,0.00030316497,0.0011105086],"category_scores_gemma":[0.00036898904,0.00013879922,0.00016788597,0.0003367322,0.00059147744,0.0002501982,0.0005566327,0.0003803012,0.00013025309],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006460077,0.000052728104,0.27429825,0.00010529596,0.00009809825,0.0027912431,0.0009208657,0.0003802041,0.7005207,0.0008059975,0.0006428816,0.018737733],"study_design_scores_gemma":[0.000014039709,0.00010989255,0.96345997,0.0000072063895,0.000028084789,0.00043568964,0.00022108902,0.0009847437,0.032413594,0.00023441977,0.0020775623,0.000013617099],"about_ca_topic_score_codex":0.002704382,"about_ca_topic_score_gemma":0.0039874823,"teacher_disagreement_score":0.002704382,"about_ca_system_score_codex":0.00033854504,"about_ca_system_score_gemma":0.00013685797,"threshold_uncertainty_score":0.0053772926},"labels":[],"label_agreement":null},{"id":"W4392602919","doi":"10.1029/2023jb028101","title":"Numerical Simulation of the Self‐Organizational Origin of Concentrically Zoned Aggregates of Siderite and Pyrite in Sediment‐Hosted Massive Sulfide Deposits","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Pyrite; Siderite; Sulfide; Sediment; Geology; Geochemistry; Iron sulfide; Mineralogy; Materials science; Sulfur; Geomorphology; Metallurgy","score_opus":0.019053129703711636,"score_gpt":0.2862103886198173,"score_spread":0.26715725891610564,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392602919","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9795823,0.00011095738,0.009784828,0.0002999803,0.000050042465,0.00006732948,0.0003892902,0.0001825112,0.009532546],"genre_scores_gemma":[0.99416524,0.00004127132,0.0045044767,0.00004156559,0.000007316792,0.00005704547,0.00017954168,0.000021883627,0.0009816994],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998895,0.000026348509,0.000005761845,0.000016841173,0.000025052097,0.000036557703],"domain_scores_gemma":[0.9989868,0.00060025003,0.00010979383,0.000046359553,0.00013627429,0.000120578836],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034829383,0.00044981643,0.00061397173,0.000472521,0.0006543894,0.00078174367,0.00096677773,0.001449881,0.0023601435],"category_scores_gemma":[0.0013709129,0.00037579972,0.0005475116,0.00048827234,0.00091501814,0.00036972758,0.0006022993,0.0005936816,0.00014837031],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000084681444,0.00009206585,0.0032057848,0.000026149759,0.000026490019,0.000102307444,0.000045165543,0.99258476,0.0014869698,0.0012001749,0.00019057667,0.00095481053],"study_design_scores_gemma":[0.000013799103,0.000012991114,0.0003882077,0.0000021937876,0.0000027385051,0.0000028779484,0.000014997695,0.9992065,0.00014438397,0.00014229119,0.00006623374,0.0000027932126],"about_ca_topic_score_codex":0.021490376,"about_ca_topic_score_gemma":0.011523924,"teacher_disagreement_score":0.021490376,"about_ca_system_score_codex":0.0011298497,"about_ca_system_score_gemma":0.0010292885,"threshold_uncertainty_score":0.04273057},"labels":[],"label_agreement":null},{"id":"W4392640329","doi":"10.1029/2022jb026180","title":"Structure and Tectonic Evolution of the NW Sulu Sea Basin (SE Asia)","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geophysical Studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Geology; Rift; Paleontology; Tectonics; Neogene; Late Miocene; Structural basin","score_opus":0.029591242588527345,"score_gpt":0.29535781433620073,"score_spread":0.2657665717476734,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392640329","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980469,0.000099065095,0.000046639816,0.000025568823,9.79386e-7,0.000001380376,0.00013080123,0.000007574849,0.0016411033],"genre_scores_gemma":[0.99932945,0.00007278961,0.00011916105,0.0000056442373,9.2903656e-7,0.0000018646741,0.00019028666,0.0000030007807,0.000276866],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999795,0.000003555273,0.000001912917,0.000005320601,0.0000042886086,0.0000054105562],"domain_scores_gemma":[0.9999268,0.00000810287,0.000022998112,0.0000054295815,0.000024446928,0.000012241773],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008196511,0.00015156333,0.0000745209,0.0007409062,0.0001748395,0.00039029715,0.00008699101,0.000082044644,0.00087848096],"category_scores_gemma":[0.000115890936,0.000095547024,0.00010026593,0.0009362502,0.00025680193,0.0001394115,0.00021203268,0.000057986555,0.00014523305],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000059879956,0.000015043854,0.95574105,0.00004744472,0.00006962605,0.00049502274,0.0014228537,0.0012954841,0.012737538,0.00067876314,0.00044328332,0.026993994],"study_design_scores_gemma":[0.000002464718,0.000012457184,0.99696046,0.000007728972,0.000010869661,0.00010956308,0.0005787939,0.0007996832,0.00043257684,0.00006147825,0.0010212169,0.0000026879345],"about_ca_topic_score_codex":0.023541925,"about_ca_topic_score_gemma":0.051221404,"teacher_disagreement_score":0.023541925,"about_ca_system_score_codex":0.00032549788,"about_ca_system_score_gemma":0.00028765845,"threshold_uncertainty_score":0.046809793},"labels":[],"label_agreement":null},{"id":"W4392655708","doi":"10.1029/2023jb027306","title":"Low δ <sup>18</sup> O and δ <sup>30</sup> Si TTG at ca. 2.3 Ga Hints at an Intraplate Rifting Onset of the Paleoproterozoic Supercontinent Cycle","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"National Key Research and Development Program of China; National Natural Science Foundation of China","keywords":"Supercontinent; Intraplate earthquake; Rift; Geology; Nuclear physics; Physics; Paleontology","score_opus":0.024218718206502923,"score_gpt":0.27977455107212357,"score_spread":0.25555583286562067,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392655708","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9944501,0.00027127424,0.0009365033,0.000043669024,0.000010418719,0.000004180952,0.0010236636,0.00011853627,0.003141679],"genre_scores_gemma":[0.99776113,0.000090318485,0.0006069731,0.000022132419,0.000003553623,0.000003178413,0.00070500886,0.000041657888,0.0007661554],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999554,0.0000013117352,0.0000024950898,0.000020907735,0.00000997465,0.000009843655],"domain_scores_gemma":[0.9999201,0.0000073794436,0.000019789928,0.000009302762,0.000029674111,0.000013757038],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011421111,0.0003129289,0.00014937336,0.0007700848,0.00035924124,0.000376368,0.00021401994,0.00022788899,0.0020298325],"category_scores_gemma":[0.00016684103,0.0001294727,0.00017101182,0.00046019797,0.00031656242,0.00018601121,0.00023521407,0.00021333438,0.00035662897],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022118531,0.000019033218,0.46047378,0.00009101551,0.000094118936,0.00042538127,0.000461537,0.0016658107,0.5175099,0.00045139468,0.0005380293,0.018048927],"study_design_scores_gemma":[0.0000050273616,0.000029311715,0.97312105,0.0000069891917,0.000032047028,0.00021903156,0.00015488811,0.0015620337,0.021406252,0.00016616768,0.0032880267,0.000009170662],"about_ca_topic_score_codex":0.017624043,"about_ca_topic_score_gemma":0.033983793,"teacher_disagreement_score":0.017624043,"about_ca_system_score_codex":0.00037907652,"about_ca_system_score_gemma":0.00023587928,"threshold_uncertainty_score":0.03504294},"labels":[],"label_agreement":null},{"id":"W4392963350","doi":"10.1029/2023jb027578","title":"Rupture Dynamics of Cascading Earthquakes in a Multiscale Fracture Network","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"King Abdullah University of Science and Technology; Southern California Earthquake Center; Directorate for Geosciences; National Aeronautics and Space Administration; National Science Foundation","keywords":"Slip (aerodynamics); Fracture (geology); Earthquake rupture; Geology; Seismology; Fault (geology); Stress field; Geotechnical engineering; Structural engineering; Engineering; Finite element method","score_opus":0.028456264270282087,"score_gpt":0.3229930380350393,"score_spread":0.29453677376475723,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392963350","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99371076,0.00004159638,0.005226793,0.000058034915,0.000004429396,0.000006328845,0.000062006744,0.00003983124,0.000850245],"genre_scores_gemma":[0.9992483,0.000016591675,0.0005983377,0.0000058570217,0.0000015526181,0.0000048682214,0.000021760708,0.0000038082685,0.000098829994],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991524,0.000013583788,0.0000053232734,0.000024897356,0.000015281186,0.000025595053],"domain_scores_gemma":[0.99958104,0.000151242,0.00011462032,0.00003219695,0.000038532165,0.00008238434],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022962074,0.0002458969,0.00032667207,0.0004703747,0.0003998177,0.00059171766,0.0005232994,0.00059005036,0.0012291074],"category_scores_gemma":[0.0010465502,0.00024615586,0.00045728651,0.0002892924,0.0006176411,0.0006194973,0.0006676313,0.00035164304,0.00006556641],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000063390755,0.00007369885,0.02304286,0.000027486325,0.00007808052,0.00031578616,0.00008992209,0.9575272,0.011876618,0.0040157437,0.0002461971,0.0026429547],"study_design_scores_gemma":[0.000009735768,0.000042545096,0.008164893,0.0000038851613,0.000014320741,0.00004252587,0.000049321276,0.98937887,0.0005735944,0.0015815134,0.00012780979,0.000011051846],"about_ca_topic_score_codex":0.0067085777,"about_ca_topic_score_gemma":0.0035966516,"teacher_disagreement_score":0.0067085777,"about_ca_system_score_codex":0.0006837603,"about_ca_system_score_gemma":0.00030045447,"threshold_uncertainty_score":0.013339102},"labels":[],"label_agreement":null},{"id":"W4392964935","doi":"10.1029/2023jb027714","title":"Fluid‐Induced Aseismic Slip May Explain the Non‐Self‐Similar Source Scaling of the Induced Earthquake Sequence Near the Dallas‐Fort Worth Airport, Texas","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Slip (aerodynamics); Scaling; Seismic moment; Induced seismicity; Geology; Seismology; Moment magnitude scale; Drop (telecommunication); Pore water pressure; Mechanics; Fault (geology); Geotechnical engineering; Engineering; Geometry; Physics; Mathematics","score_opus":0.06280816725862677,"score_gpt":0.3229982099822097,"score_spread":0.2601900427235829,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392964935","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99683833,0.000025585152,0.0020975792,0.000065700246,0.000003991712,0.000005960677,0.0000478844,0.000029850578,0.00088489224],"genre_scores_gemma":[0.9997061,0.000009442039,0.0001699461,0.000003506857,0.0000014735265,0.000002005468,0.000020676107,0.0000019376882,0.000084849686],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999691,0.0000039542447,0.000002590192,0.000008764354,0.000003985668,0.000011580979],"domain_scores_gemma":[0.99986804,0.000017734223,0.000056228837,0.0000132346495,0.000018716055,0.000025973346],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008258839,0.00027188123,0.00017182447,0.00030764448,0.00026611888,0.00040132913,0.00041810758,0.00037319356,0.0011176676],"category_scores_gemma":[0.00043078823,0.0001496345,0.00025466894,0.00016751324,0.00033878995,0.00032850594,0.0002939835,0.00025323316,0.000090313886],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013607022,0.0002365643,0.2079939,0.00005528523,0.00008217811,0.0009836216,0.00021694847,0.7369028,0.043654088,0.0040685423,0.00057898485,0.0050909915],"study_design_scores_gemma":[0.000018971261,0.00005155684,0.06447778,0.0000059082395,0.000013064335,0.00007082639,0.00010999442,0.93275166,0.0016367106,0.00064122875,0.00021217272,0.000010233797],"about_ca_topic_score_codex":0.00868905,"about_ca_topic_score_gemma":0.0054888735,"teacher_disagreement_score":0.00868905,"about_ca_system_score_codex":0.0005755564,"about_ca_system_score_gemma":0.00026046616,"threshold_uncertainty_score":0.017276943},"labels":[],"label_agreement":null},{"id":"W4394916919","doi":"10.1029/2023jb028226","title":"Evaluating the Rheological Controls on Topography Development During Craton Stabilization: Objective Approaches to Comparing Geodynamic Models","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Rheology; Geology; Craton; Physics; Thermodynamics; Paleontology","score_opus":0.25028573304626384,"score_gpt":0.35835939389814436,"score_spread":0.10807366085188053,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4394916919","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9748887,0.00006560089,0.021513484,0.000059192713,0.000005229219,0.00010296089,0.0007240567,0.00017694902,0.0024638383],"genre_scores_gemma":[0.99222386,0.000027091242,0.007069873,0.00001186562,0.0000034135137,0.00010415654,0.00034680776,0.000039084076,0.0001738619],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9992555,0.00039161433,0.000059091384,0.000101584534,0.00012621174,0.00006594855],"domain_scores_gemma":[0.9971842,0.0016446988,0.00042361915,0.00029529727,0.00033611082,0.00011598533],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0033410406,0.0010420752,0.0006521033,0.0024595556,0.00041160907,0.0022242279,0.0007322053,0.0007525922,0.001088654],"category_scores_gemma":[0.0055795256,0.00037824505,0.0009155274,0.0009834644,0.00067670876,0.0008218678,0.0011949218,0.00062369404,0.00011959332],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025412274,0.00026760148,0.04987685,0.00007302726,0.0003029547,0.00004992971,0.00013167303,0.93315166,0.004270931,0.0016888459,0.00021208017,0.009720356],"study_design_scores_gemma":[0.000021123878,0.00012384186,0.012359185,0.000010788167,0.00002362121,0.0000069113307,0.00012738866,0.9848587,0.0016937825,0.00062630797,0.00012914916,0.000019263614],"about_ca_topic_score_codex":0.009782486,"about_ca_topic_score_gemma":0.008073061,"teacher_disagreement_score":0.009782486,"about_ca_system_score_codex":0.0013514258,"about_ca_system_score_gemma":0.0007287533,"threshold_uncertainty_score":0.019451082},"labels":[],"label_agreement":null},{"id":"W4395052655","doi":"10.1029/2024jb029251","title":"Thank You to Our 2023 Reviewers","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Research Data Management Practices","field":"Computer Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Psychology","score_opus":0.17022617126221015,"score_gpt":0.4806437028503916,"score_spread":0.3104175315881814,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4395052655","genre_codex":"editorial","genre_gemma":"editorial","domain_codex":null,"domain_gemma":"evaluation","model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"editorial","genre_consensus":"editorial","domain_candidate":"evaluation","domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00034004258,0.008616145,0.002569333,0.12225545,0.8499072,0.0004094677,0.0009383255,0.0018286481,0.0131354155],"genre_scores_gemma":[0.006427744,0.012110268,0.0077746413,0.14751038,0.5965154,0.0011736532,0.002204348,0.0040496015,0.22223398],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9710958,0.0063385777,0.0033385362,0.0039127935,0.01401312,0.0013012683],"domain_scores_gemma":[0.6737012,0.014006582,0.010817418,0.006245474,0.27209854,0.023130732],"candidate_categories":["metaresearch"],"consensus_categories":[],"category_scores_codex":[0.021725515,0.0028238762,0.002580461,0.007118058,0.0051022866,0.021679096,0.0032144499,0.006648998,0.11967417],"category_scores_gemma":[0.15146755,0.0012000547,0.0021288747,0.0030960464,0.002003624,0.0070716524,0.004238563,0.007282297,0.1754938],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012837889,0.0000040366945,0.00007255639,0.00008160731,0.000004764565,0.00004768076,0.000048381535,0.000010401369,0.00006673984,0.00014893485,0.99070096,0.008801104],"study_design_scores_gemma":[0.0000105620775,0.000010258765,0.0001532119,0.0001968295,0.000009023194,0.00017287052,0.00018410238,0.000043091117,0.00007446557,0.00036020653,0.9987601,0.000025258312],"about_ca_topic_score_codex":0.002090398,"about_ca_topic_score_gemma":0.0041094725,"teacher_disagreement_score":0.97827446,"about_ca_system_score_codex":0.0038560722,"about_ca_system_score_gemma":0.009699976,"threshold_uncertainty_score":0.40034997},"labels":[],"label_agreement":null},{"id":"W4396494611","doi":"10.1029/2023jb027769","title":"Influence of GIA Uncertainty on Climate Model Evaluation With GRACE/GRACE‐FO Satellite Gravimetry Data","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Bundesministerium für Bildung und Forschung; Deutsche Forschungsgemeinschaft","keywords":"Post-glacial rebound; Climatology; Environmental science; Climate change; Satellite; Gravitational field; Water storage; Gravimetry; Physical geography; Meteorology; Geology; Geography; Sea level; Geomorphology","score_opus":0.12294153734316095,"score_gpt":0.38620991509119235,"score_spread":0.2632683777480314,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4396494611","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9823382,0.00035721654,0.009636452,0.0005691957,0.00010137314,0.00007757286,0.0026610803,0.00062453264,0.003634273],"genre_scores_gemma":[0.9962381,0.000039058094,0.0024437841,0.00008729367,0.000017210878,0.000030619267,0.0009187757,0.00008502149,0.00014006451],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9973968,0.0015239262,0.0002043352,0.0003814165,0.00031308085,0.00018041085],"domain_scores_gemma":[0.9900893,0.006245462,0.0008611388,0.0012296976,0.0012364606,0.00033793892],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.010940763,0.00094202434,0.00070153666,0.0007905742,0.0006905362,0.001819304,0.0011029878,0.0009243209,0.00070003065],"category_scores_gemma":[0.018774975,0.00038456547,0.0015156571,0.0010353171,0.00080425414,0.0013397156,0.0011275492,0.0011701743,0.00020444315],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00071632705,0.000094504816,0.05372184,0.000062588675,0.00046739684,0.00009837992,0.000047739486,0.93393666,0.0020269847,0.00084778265,0.00097630935,0.0070034782],"study_design_scores_gemma":[0.00013749549,0.000108131404,0.029976116,0.000030413712,0.00018135563,0.000027932358,0.00005151412,0.9638582,0.004190599,0.00052581745,0.0008565755,0.00005601561],"about_ca_topic_score_codex":0.044102058,"about_ca_topic_score_gemma":0.01676464,"teacher_disagreement_score":0.044102058,"about_ca_system_score_codex":0.0014770833,"about_ca_system_score_gemma":0.0011162619,"threshold_uncertainty_score":0.08769071},"labels":[],"label_agreement":null},{"id":"W4396832141","doi":"10.1029/2024jb028735","title":"Next Generation Seismic Source Detection by Computer Vision: Untangling the Complexity of the 2016 Kaikōura Earthquake Sequence","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismology and Earthquake Studies","field":"Computer Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; Ocean Networks Canada Society; University of Victoria; Geological Survey of Canada","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; University of Victoria","keywords":"Sequence (biology); Seismology; Geology; Computer science","score_opus":0.10801890338709146,"score_gpt":0.34979906148387285,"score_spread":0.24178015809678138,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4396832141","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7827983,0.0003020763,0.21101277,0.00041865231,0.00006351716,0.000065088825,0.00042397183,0.0014284672,0.0034871448],"genre_scores_gemma":[0.82819855,0.00011632316,0.17013016,0.000048868926,0.000024729054,0.000016579233,0.00067467004,0.000062373365,0.00072772143],"study_design_codex":"design_other","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99984586,0.000017150358,0.000008526932,0.000046271714,0.000048719015,0.000033364075],"domain_scores_gemma":[0.9995704,0.00011353067,0.000067018176,0.00006112535,0.00013780774,0.000050129376],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035903326,0.00038712518,0.00027467954,0.0026181245,0.00022635882,0.0006915188,0.00036099777,0.00029462687,0.0005911435],"category_scores_gemma":[0.0009654334,0.00016028425,0.00035450122,0.0010412749,0.00028855307,0.00052997255,0.00058712286,0.0004014766,0.00024318996],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00051684683,0.0002452178,0.053583574,0.00011878817,0.000091690636,0.0004557796,0.0005592765,0.06805015,0.14499412,0.0026608661,0.003974474,0.7247492],"study_design_scores_gemma":[0.000020656436,0.000094817115,0.07168545,0.000015029237,0.00004547952,0.00019010511,0.0002718493,0.8871749,0.03468982,0.0027864696,0.0029912067,0.000034301273],"about_ca_topic_score_codex":0.0087701585,"about_ca_topic_score_gemma":0.017110135,"teacher_disagreement_score":0.0087701585,"about_ca_system_score_codex":0.0003592224,"about_ca_system_score_gemma":0.0005601464,"threshold_uncertainty_score":0.017438233},"labels":[],"label_agreement":null},{"id":"W4398205129","doi":"10.1029/2024jb028752","title":"Incipient Subduction and Slip Partitioning at High Obliquity: The Haida Gwaii Plate Boundary","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University; Geological Survey of Canada; Natural Resources Canada; University of Victoria; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Subduction; Geology; Seismology; Slip (aerodynamics); Plate tectonics; Engineering; Aerospace engineering; Tectonics","score_opus":0.04314574524424953,"score_gpt":0.316515748697,"score_spread":0.2733700034527505,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4398205129","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99889934,0.000024611802,0.000060122547,0.00002430962,0.0000021258531,0.000004162147,0.000118659314,0.0000064334763,0.00086024473],"genre_scores_gemma":[0.99941194,0.000015496731,0.000089179906,0.000005964389,0.0000018991202,0.0000030064714,0.000208498,0.0000022936267,0.00026163433],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993503,0.0000035762591,0.0000035480596,0.00001900095,0.000018642968,0.000020215186],"domain_scores_gemma":[0.99976736,0.000017596589,0.00007356952,0.00001988171,0.0000547234,0.00006697438],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000097879354,0.00021463445,0.00020470805,0.0010802227,0.00059608044,0.0007158765,0.0002052782,0.00027546185,0.0010647253],"category_scores_gemma":[0.00040952762,0.00021611544,0.00012277487,0.0010794053,0.0006152584,0.0002949155,0.00065876084,0.00026327296,0.00016522275],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011865353,0.00002812364,0.97616553,0.00003231848,0.000034538083,0.000999752,0.0013380642,0.002163062,0.009624369,0.00026771415,0.0006114078,0.008616367],"study_design_scores_gemma":[0.0000035353262,0.000007439539,0.9975967,0.0000054637585,0.0000055101154,0.000057878027,0.0003899897,0.0014036591,0.00021284432,0.000038699854,0.00027423297,0.000004121961],"about_ca_topic_score_codex":0.11173217,"about_ca_topic_score_gemma":0.21426784,"teacher_disagreement_score":0.8882678,"about_ca_system_score_codex":0.0010134942,"about_ca_system_score_gemma":0.0007556277,"threshold_uncertainty_score":0.22216368},"labels":[],"label_agreement":null},{"id":"W4398208950","doi":"10.1029/2023jb027012","title":"High‐Resolution Mantle Transition Zone Imaging Using Multi‐Dimensional Reconstruction of SS Precursors","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta; Geological Survey of Canada; Natural Resources Canada","funders":"Fundamental Research Funds for the Central Universities; National Natural Science Foundation of China","keywords":"Transition zone; Geology; Mantle (geology); High resolution; Seismology; Remote sensing; Geophysics","score_opus":0.03505399528567535,"score_gpt":0.31276024940219277,"score_spread":0.2777062541165174,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4398208950","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6216532,0.00039887519,0.37003517,0.00028947875,0.00005943463,0.00008064684,0.001547529,0.0019298361,0.004005874],"genre_scores_gemma":[0.8158468,0.00024087616,0.18083394,0.00004897688,0.0000246876,0.000040707513,0.0019069907,0.00013528805,0.0009217327],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998896,0.000016436432,0.000006326804,0.000020339769,0.00004980253,0.000017470416],"domain_scores_gemma":[0.9997712,0.000043041666,0.000038589325,0.0000456084,0.00007558688,0.00002606236],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026172528,0.0006388434,0.00027949671,0.0008507748,0.00015918292,0.0006778451,0.00045306367,0.00038747874,0.001523003],"category_scores_gemma":[0.00076164544,0.00025771654,0.00036741156,0.0007533492,0.0002373674,0.00053176127,0.0006065056,0.00048085954,0.000421764],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005568211,0.00021293959,0.027211668,0.00042277257,0.00015837613,0.000977816,0.0004668386,0.28581586,0.5253233,0.0048490483,0.0028262017,0.15117842],"study_design_scores_gemma":[0.000041789845,0.00010581894,0.01166204,0.00002001503,0.000036172994,0.00019762982,0.00015376654,0.92384034,0.05919827,0.0017558286,0.0029383376,0.000049943632],"about_ca_topic_score_codex":0.002320664,"about_ca_topic_score_gemma":0.0034067933,"teacher_disagreement_score":0.002320664,"about_ca_system_score_codex":0.00014480368,"about_ca_system_score_gemma":0.00050550787,"threshold_uncertainty_score":0.005094886},"labels":[],"label_agreement":null},{"id":"W4399883802","doi":"10.1029/2023jb028014","title":"Depth‐Dependent Anisotropy Along Northwest Segment of the North Anatolian Fault Zone: Evidence for Paleo‐Tectonic Structures Contributing to Overall Complexity","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"Bilimsel Araştırma Projeleri Birimi, İstanbul Teknik Üniversitesi","keywords":"Geology; Seismology; Seismic anisotropy; Crust; Anisotropy; Shear zone; North Anatolian Fault; Tectonics; Mantle (geology); Receiver function; Shear (geology); Lithosphere; Geophysics; Petrology","score_opus":0.07277847746761351,"score_gpt":0.35844469306906696,"score_spread":0.28566621560145344,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399883802","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992717,0.000049877854,0.00011342251,0.00001101471,7.348404e-7,0.0000015611963,0.00010819911,0.0000063567522,0.0004371589],"genre_scores_gemma":[0.99969625,0.000027247543,0.00008337238,0.0000016630635,8.5097133e-7,0.0000013358734,0.000099815945,0.0000017316296,0.00008787155],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994814,0.0000062671616,0.0000051739926,0.000016193086,0.000010643867,0.000013632279],"domain_scores_gemma":[0.9998485,0.000023255872,0.000053004194,0.000016109809,0.00004092996,0.00001822857],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000104888575,0.00016839677,0.00016168912,0.0011174132,0.00023000398,0.00049527176,0.00014890393,0.00018499242,0.0011308732],"category_scores_gemma":[0.00025640483,0.00016283248,0.00012254118,0.0008494371,0.0002778799,0.00023056344,0.00026693888,0.000115635165,0.00016548875],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013360455,0.000031460168,0.9256382,0.000031856518,0.00008146461,0.00020413786,0.00046640553,0.0016356441,0.059377108,0.00022601367,0.00011577042,0.012058368],"study_design_scores_gemma":[0.0000011235525,0.0000030927783,0.9983399,0.0000016702722,0.000004899592,0.000031572883,0.000081750564,0.0011349911,0.00030714215,0.000024997104,0.000067194764,0.0000016785071],"about_ca_topic_score_codex":0.018307004,"about_ca_topic_score_gemma":0.02744774,"teacher_disagreement_score":0.018307004,"about_ca_system_score_codex":0.00030149063,"about_ca_system_score_gemma":0.00020781552,"threshold_uncertainty_score":0.036400855},"labels":[],"label_agreement":null},{"id":"W4400123625","doi":"10.1029/2023jb027238","title":"A Hybrid Normal Mode‐Collocation Method for Finding the Response of Laterally Homogeneous Compressible Maxwell Viscoelastic Earth Models","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Collocation (remote sensing); Mathematical analysis; Viscoelasticity; Mathematics; Laplace transform; Collocation method; Amplitude; Piecewise; Normal mode; Physics; Vibration; Geology; Optics; Differential equation; Acoustics","score_opus":0.07490070762874373,"score_gpt":0.36448043337830294,"score_spread":0.2895797257495592,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400123625","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.040061172,0.000033517368,0.95800805,0.000031154534,0.000010279937,0.00003634572,0.000054629385,0.00064969633,0.0011152225],"genre_scores_gemma":[0.48944458,0.00005519215,0.507627,0.000042671854,0.000013445977,0.00012302691,0.00018711247,0.00026244027,0.0022444967],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998741,0.000048707378,0.0000066305774,0.000021291182,0.000036260826,0.000012986201],"domain_scores_gemma":[0.9995042,0.00023592231,0.000041606167,0.00004951803,0.00014154914,0.000027239059],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004920198,0.0006395202,0.0003385707,0.00052497524,0.00032368943,0.00037963747,0.00079841603,0.00062054116,0.0023922771],"category_scores_gemma":[0.0016390254,0.00038758677,0.0004289628,0.00026416808,0.00023454739,0.000371602,0.0005691189,0.00042668817,0.00048068014],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006093652,0.00004633998,0.0017275088,0.000041625655,0.000032621945,0.00009277666,0.00010320258,0.9195326,0.010251387,0.00332534,0.0006585564,0.064127125],"study_design_scores_gemma":[0.0000021343299,0.0000037258783,0.000063559186,0.0000010161283,7.3365703e-7,0.0000025979339,0.0000036843533,0.9992679,0.00026665337,0.00024538572,0.00014065912,0.0000019874649],"about_ca_topic_score_codex":0.011915415,"about_ca_topic_score_gemma":0.010755986,"teacher_disagreement_score":0.011915415,"about_ca_system_score_codex":0.0003772529,"about_ca_system_score_gemma":0.00074458256,"threshold_uncertainty_score":0.023692131},"labels":[],"label_agreement":null},{"id":"W4400735353","doi":"10.1029/2023jb028194","title":"Clumped Isotope Signatures of Abiotic Methane: The Role of the Combinatorial Isotope Effect","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Nuclear Safety and Security Commission; National Aeronautics and Space Administration","keywords":"Abiogenic petroleum origin; Methane; Chemistry; Isotopes of carbon; Carbon fibers; Hydrogen; Hydrothermal circulation; Carbon dioxide; Isotope fractionation; Carbon monoxide; Kinetic isotope effect; Analytical Chemistry (journal); Fractionation; Deuterium; Environmental chemistry; Organic chemistry; Chemical engineering; Materials science; Total organic carbon; Catalysis","score_opus":0.010404680472068105,"score_gpt":0.2956522619690098,"score_spread":0.2852475814969417,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400735353","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9953185,0.00022818397,0.0032003017,0.00003137103,0.000008129057,0.0000073855213,0.00016274309,0.00005340078,0.0009898974],"genre_scores_gemma":[0.99928194,0.000026493233,0.00048571973,0.000010964778,0.0000017936898,0.0000040093055,0.000045220848,0.000006506479,0.00013734584],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99989307,0.000008780695,0.000006275794,0.00003701333,0.000029146642,0.000025662039],"domain_scores_gemma":[0.9997161,0.000101247104,0.000059675156,0.00005047438,0.000037713467,0.00003480589],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017829119,0.00020360666,0.00017817835,0.00040296608,0.00019060205,0.0003628281,0.0002449256,0.0001758775,0.0012345397],"category_scores_gemma":[0.00053471274,0.00019456606,0.00008733769,0.00024418134,0.0006436911,0.00025080293,0.00035006177,0.00019529334,0.00011630908],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021365522,0.00001422193,0.021338038,0.000048002083,0.000016242991,0.00010914304,0.00003548746,0.0003580658,0.9746791,0.00036251414,0.000029886802,0.0027956064],"study_design_scores_gemma":[0.000017105447,0.00018309207,0.17631423,0.000010548275,0.000030374991,0.00034582854,0.0001344028,0.007244568,0.8132229,0.0010724835,0.001398314,0.000026196094],"about_ca_topic_score_codex":0.00084080163,"about_ca_topic_score_gemma":0.0015864974,"teacher_disagreement_score":0.0012345397,"about_ca_system_score_codex":0.0003075577,"about_ca_system_score_gemma":0.00012505827,"threshold_uncertainty_score":0.004129946},"labels":[],"label_agreement":null},{"id":"W4401007555","doi":"10.1029/2024jb028791","title":"Linear Array Double Difference Adjoint Ambient Noise Tomography of the Central Tanlu Fault Zone, Eastern China","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"China Earthquake Administration; University of Science and Technology of China; National Natural Science Foundation of China","keywords":"Fault (geology); Geology; Ambient noise level; Seismology; Noise (video); Tomography; China; Geodesy; Geography; Physics; Computer science; Geomorphology; Archaeology; Sound (geography); Artificial intelligence; Optics","score_opus":0.027272576692018703,"score_gpt":0.29435992559562335,"score_spread":0.26708734890360464,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401007555","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99355245,0.00004025585,0.005458441,0.000037501544,0.0000073205015,0.0000058010255,0.00016159198,0.00006903065,0.00066765014],"genre_scores_gemma":[0.9972011,0.000012963199,0.002408573,0.0000070193933,0.0000035554306,0.0000038421963,0.000121017176,0.0000042677134,0.00023771123],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991167,0.0000116897645,0.0000051413117,0.000029693167,0.000021641312,0.000020136766],"domain_scores_gemma":[0.9998466,0.000021735294,0.000034927016,0.000017681356,0.000060837454,0.000018329014],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021196922,0.00036008662,0.00020291943,0.000725145,0.00018147295,0.000338794,0.00026267947,0.00020689006,0.00053612073],"category_scores_gemma":[0.00046636187,0.00013293947,0.00014589999,0.0007455297,0.00024491883,0.00023136103,0.00034419447,0.00014123159,0.00007883307],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007013423,0.0002735256,0.48521975,0.00016667333,0.00013658404,0.0010555428,0.0011062991,0.14718734,0.21557753,0.0016234296,0.0009064167,0.14604563],"study_design_scores_gemma":[0.00007532252,0.00014140776,0.56394714,0.000022918413,0.00007646359,0.00021775399,0.00041688426,0.41572672,0.017321413,0.0007010146,0.001302438,0.000050545328],"about_ca_topic_score_codex":0.017468516,"about_ca_topic_score_gemma":0.032580823,"teacher_disagreement_score":0.017468516,"about_ca_system_score_codex":0.00026387203,"about_ca_system_score_gemma":0.0006233473,"threshold_uncertainty_score":0.034733653},"labels":[],"label_agreement":null},{"id":"W4401639492","doi":"10.1029/2024jb029159","title":"Spatial Distribution of Tremor Episodes From Long‐Term Monitoring in the Northern Cascadia Subduction Zone","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Victoria","funders":"","keywords":"Subduction; Geology; Term (time); Seismology; Episodic tremor and slip; Spatial distribution; Remote sensing; Tectonics","score_opus":0.04535060136841667,"score_gpt":0.3246652609147982,"score_spread":0.2793146595463815,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401639492","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99814296,0.000062576175,0.00012515885,0.000011510393,9.840682e-7,0.000003648416,0.0011502893,0.000025543475,0.00047734648],"genre_scores_gemma":[0.9979754,0.00004222345,0.00010227011,0.000002612144,0.0000023236014,0.000004876559,0.0017110108,0.0000035159123,0.00015568578],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99977547,0.000022535087,0.000026230959,0.00007516948,0.00006561634,0.00003496986],"domain_scores_gemma":[0.99891734,0.00016029482,0.0003879727,0.0001104421,0.00021639689,0.00020758674],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037671113,0.00023722553,0.00021008511,0.0022746832,0.0003176853,0.000509998,0.00029569454,0.00024471368,0.0007245606],"category_scores_gemma":[0.0010594093,0.00013445463,0.00030427775,0.0021443826,0.00027232774,0.00019205107,0.00060025515,0.00016515708,0.00016696008],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005354793,0.000012586502,0.99014306,0.000028394918,0.00009318383,0.00013593408,0.00036126282,0.0015859896,0.0026938152,0.000022967684,0.0001834112,0.004685805],"study_design_scores_gemma":[9.242431e-7,0.000007096221,0.9991881,0.0000026570685,0.000008110587,0.000023901624,0.00006866283,0.0005004516,0.00008259428,0.000004601505,0.00011118198,0.0000017850592],"about_ca_topic_score_codex":0.056853965,"about_ca_topic_score_gemma":0.09306732,"teacher_disagreement_score":0.056853965,"about_ca_system_score_codex":0.0006181667,"about_ca_system_score_gemma":0.00031014712,"threshold_uncertainty_score":0.11304605},"labels":[],"label_agreement":null},{"id":"W4402232958","doi":"10.1029/2024jb029104","title":"Strong Lg‐Wave Attenuation Reveals Quarter‐Toroidal Crustal Melting Around the Yakutat Terrane in South‐Central Alaska","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"China Postdoctoral Science Foundation; National Natural Science Foundation of China","keywords":"Terrane; Attenuation; Quarter (Canadian coin); Seismology; Geology; Toroid; Physics; Geography; Tectonics; Nuclear physics; Optics; Archaeology","score_opus":0.05875102686652766,"score_gpt":0.3251521146795741,"score_spread":0.26640108781304644,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402232958","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99867046,0.000041252155,0.0003976778,0.000031557087,0.0000028264492,0.0000018903595,0.00015782546,0.000060673126,0.00063587405],"genre_scores_gemma":[0.9995017,0.000020097534,0.00020182072,0.0000042792203,0.0000018512445,0.0000015925567,0.0001296964,0.000005196293,0.00013364403],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996233,0.000003501556,0.00000200169,0.000012622148,0.0000068337613,0.000012771664],"domain_scores_gemma":[0.9999355,0.000008939403,0.000013681585,0.0000076213933,0.000018176343,0.00001610227],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009043212,0.00026308,0.00022240491,0.00044449474,0.0003725514,0.00045996965,0.00026175697,0.00034501564,0.0013600029],"category_scores_gemma":[0.00020440943,0.00022417684,0.00020903492,0.0004133045,0.00027128728,0.00024825186,0.000358804,0.00024456417,0.000247679],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031749162,0.00013368133,0.8412095,0.00007892451,0.00013820673,0.00094109005,0.001036515,0.039972477,0.09683454,0.00026476555,0.0006985545,0.018374301],"study_design_scores_gemma":[0.000015259728,0.00004510188,0.9360519,0.000011152049,0.00004461364,0.00013252033,0.00067036494,0.0606458,0.0018578854,0.00010865009,0.0003998205,0.000016871512],"about_ca_topic_score_codex":0.035306007,"about_ca_topic_score_gemma":0.037028573,"teacher_disagreement_score":0.035306007,"about_ca_system_score_codex":0.00023694974,"about_ca_system_score_gemma":0.00027088847,"threshold_uncertainty_score":0.07020098},"labels":[],"label_agreement":null},{"id":"W4402274891","doi":"10.1029/2024jb029253","title":"A 3‐D Seismic Tomographic Study of Spreading Structures and Smooth Seafloor Generated by Detachment Faulting—The Ultra‐Slow Spreading Southwest Indian Ridge at 64°30′E","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Institut Polaire Français Paul Emile Victor; Agence Nationale de la Recherche","keywords":"Geology; Seafloor spreading; Detachment fault; Magmatism; Tectonics; Seismology; Bathymetry; Lithology; Mid-Atlantic Ridge; Ridge; Volcano; Mid-ocean ridge; Magma chamber; Mantle (geology); Ridge push; Transform fault; Petrology; Lithosphere; Geophysics; Magma; Paleontology; Hydrothermal circulation","score_opus":0.027809278758774796,"score_gpt":0.30517472304389026,"score_spread":0.27736544428511545,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402274891","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99946934,0.000007701531,0.00009596615,0.000008483803,7.1386745e-7,0.0000028240524,0.00014734924,0.000014080794,0.00025351945],"genre_scores_gemma":[0.99923146,0.000010119624,0.0003428157,0.0000036780546,0.0000017374081,0.000002619438,0.00030898568,0.000004815853,0.00009379741],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999567,0.0000042934585,0.0000024424717,0.000010915333,0.000011885171,0.00001369894],"domain_scores_gemma":[0.999866,0.00001951339,0.000035019417,0.000012851411,0.000025803582,0.00004079997],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007602755,0.00024723666,0.00018025697,0.00089709315,0.00030417362,0.00035761407,0.00030741698,0.0002243691,0.0005763052],"category_scores_gemma":[0.0002103852,0.00024366229,0.00036580182,0.0006624761,0.00026512082,0.00013146282,0.00028082263,0.00019403287,0.00011160104],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044518014,0.00026350655,0.83860224,0.00005905093,0.00017614377,0.00168273,0.0012752672,0.023733834,0.112273745,0.00026095894,0.00065831136,0.020568976],"study_design_scores_gemma":[0.0000135915525,0.000033085147,0.98368025,0.000004196228,0.000020327068,0.000119671786,0.0002649576,0.014566382,0.001001648,0.000023569131,0.0002619562,0.0000103177845],"about_ca_topic_score_codex":0.04854345,"about_ca_topic_score_gemma":0.08871679,"teacher_disagreement_score":0.04854345,"about_ca_system_score_codex":0.00045077922,"about_ca_system_score_gemma":0.0004114425,"threshold_uncertainty_score":0.096521795},"labels":[],"label_agreement":null},{"id":"W4402572682","doi":"10.1029/2024jb028691","title":"How Induced Earthquakes Respond to Pre‐Existing Fractures and Hydraulic Fracturing Operations? A Case Study in South China","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Fundamental Research Funds for the Central Universities; Higher Education Discipline Innovation Project; Dalhousie University; Canada Foundation for Innovation; National Natural Science Foundation of China; Ocean Frontier Institute; China Scholarship Council","keywords":"Hydraulic fracturing; China; Geology; Geotechnical engineering; Seismology; Petroleum engineering; Forensic engineering; Engineering; Geography","score_opus":0.0707356037291648,"score_gpt":0.3750260418518048,"score_spread":0.30429043812264,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402572682","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99884015,0.000054435353,0.00044286516,0.000119124175,0.0000029107164,0.000010663339,0.00011705999,0.000011124394,0.00040175204],"genre_scores_gemma":[0.9987897,0.00007755041,0.0006126221,0.000015663576,0.000004778305,0.000006727818,0.00012884117,0.0000034988711,0.00036070053],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997863,0.000042914602,0.00001741103,0.000042197124,0.000043312728,0.00006791135],"domain_scores_gemma":[0.9994659,0.0001709303,0.00009930184,0.00005276004,0.00010645387,0.00010482264],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005300258,0.000363209,0.0002493093,0.0010708694,0.00072969036,0.0004544264,0.0005773566,0.0006810137,0.00089307793],"category_scores_gemma":[0.0009432035,0.00018277309,0.0004381408,0.0014738482,0.00065045967,0.00049648416,0.00052426994,0.00026537268,0.000095865624],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027881167,0.00036400137,0.87613946,0.00023972003,0.0001739927,0.022736777,0.0053387457,0.042541012,0.009431638,0.0016747601,0.0017677557,0.039313268],"study_design_scores_gemma":[0.000049900053,0.00022665366,0.87201804,0.000051619103,0.00016685796,0.0012761999,0.016401479,0.10168489,0.0032734228,0.00152648,0.0032467674,0.00007768679],"about_ca_topic_score_codex":0.080961615,"about_ca_topic_score_gemma":0.14003056,"teacher_disagreement_score":0.080961615,"about_ca_system_score_codex":0.001419128,"about_ca_system_score_gemma":0.0010125692,"threshold_uncertainty_score":0.16098076},"labels":[],"label_agreement":null},{"id":"W4402694859","doi":"10.1029/2024jb029387","title":"A Reference Model of Crustal Thickness and <i>V</i><sub><i>p</i></sub>/<i>V</i><sub><i>s</i></sub> of Western Canada","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary; University of Alberta; University of Ottawa","funders":"","keywords":"Geology; Geodesy; Geometry; Mathematics","score_opus":0.03338480330981208,"score_gpt":0.27936204791538355,"score_spread":0.24597724460557147,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402694859","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.90487796,0.000378685,0.06900441,0.00025697282,0.000023123253,0.00006411174,0.00961033,0.0010422129,0.014742268],"genre_scores_gemma":[0.985408,0.00017145791,0.008045572,0.000018984625,0.000003905813,0.00004560842,0.0027684218,0.000041745407,0.0034962958],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989915,0.0000075608855,0.0000033886229,0.000044673743,0.000020634376,0.00002466448],"domain_scores_gemma":[0.99982977,0.000022097236,0.000020469995,0.000020517957,0.00008805358,0.000019001342],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012598552,0.00057703594,0.00023941004,0.00055287825,0.00057587,0.00084710756,0.0016020454,0.0004894515,0.0019397866],"category_scores_gemma":[0.0005105063,0.00030314302,0.00040246625,0.0009659054,0.00045714597,0.00045991797,0.00023333599,0.00028416526,0.00045084002],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000034086093,0.000014674023,0.013982043,0.000016314076,0.0000319663,0.00004823386,0.00004372198,0.97467065,0.001640239,0.002290097,0.0007389362,0.0064891865],"study_design_scores_gemma":[0.000015061754,0.000010034699,0.007442044,0.0000061501023,0.000019972887,0.000019122692,0.000041165298,0.9892783,0.00067056203,0.0008689282,0.0016159936,0.000012727119],"about_ca_topic_score_codex":0.86579645,"about_ca_topic_score_gemma":0.7473204,"teacher_disagreement_score":0.13420355,"about_ca_system_score_codex":0.0070045814,"about_ca_system_score_gemma":0.006192048,"threshold_uncertainty_score":0.26998776},"labels":[],"label_agreement":null},{"id":"W4403250483","doi":"10.1029/2023jb028250","title":"Vertical Displacements and Sea‐Level Changes in Eastern North America Driven by Glacial Isostatic Adjustment: An Ensemble Modeling Approach","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey; National Science Foundation","keywords":"Post-glacial rebound; Glacial period; Geology; Sea level; Climatology; Geodesy; Last Glacial Maximum; Sea level rise; Physical geography; Oceanography; Geomorphology; Climate change; Geography","score_opus":0.08770298380581455,"score_gpt":0.3281144225648313,"score_spread":0.24041143875901677,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403250483","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9875301,0.00013037458,0.010869991,0.00010222675,0.000019676881,0.000014079542,0.0004729715,0.0001182224,0.00074234983],"genre_scores_gemma":[0.99458647,0.00011641395,0.0039907903,0.0000271863,0.000021632786,0.000032392007,0.0008180951,0.000027635208,0.00037948947],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99981505,0.000064868305,0.000012456829,0.00005838134,0.000023393695,0.000025841347],"domain_scores_gemma":[0.99922204,0.0004182395,0.00009632241,0.000088050256,0.000112904265,0.00006238848],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010286816,0.0006729109,0.00084945845,0.0009080431,0.00062504783,0.0008165497,0.0009131221,0.00082082796,0.00080695207],"category_scores_gemma":[0.0017261993,0.0004486897,0.0016537989,0.0008214587,0.00026540965,0.00081632956,0.000599477,0.0006393249,0.00011245918],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000032314518,0.00004591475,0.02590104,0.00000925438,0.00023610049,0.000033883025,0.000033088534,0.9689547,0.00039947178,0.00023782316,0.00020759099,0.0039087893],"study_design_scores_gemma":[0.0000035965659,0.000010687365,0.0036587005,0.0000023118514,0.000023830104,0.0000035269213,0.000011199771,0.99600923,0.00006228136,0.00013708648,0.00007204033,0.000005569482],"about_ca_topic_score_codex":0.07676906,"about_ca_topic_score_gemma":0.056706488,"teacher_disagreement_score":0.92323095,"about_ca_system_score_codex":0.00067972695,"about_ca_system_score_gemma":0.0008704263,"threshold_uncertainty_score":0.1526444},"labels":[],"label_agreement":null},{"id":"W4403352447","doi":"10.1029/2023jb028370","title":"Passive Source Reverse Time Migration Based on the Spectral Element Method","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"University of Texas at Dallas; University of Toronto; Natural Sciences and Engineering Research Council of Canada; Discovery Eye Foundation; National Science Foundation","keywords":"Seismic migration; Element (criminal law); Computer science; Geology; Seismology; Political science","score_opus":0.030012271823634175,"score_gpt":0.32899675009025225,"score_spread":0.29898447826661806,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403352447","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.013062223,0.000020901765,0.985587,0.000031740565,0.000020630809,0.00002339617,0.000025533267,0.00026550135,0.0009630955],"genre_scores_gemma":[0.15582065,0.000081963815,0.83981687,0.000040564046,0.00002135637,0.00011719989,0.00018281548,0.00009646717,0.0038222028],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99990606,0.000023530012,0.0000057196203,0.000016509566,0.000039096052,0.00000911697],"domain_scores_gemma":[0.9997956,0.0000621489,0.000025370417,0.000029362467,0.000076093216,0.000011518812],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020134983,0.0006348826,0.0003023726,0.0004892337,0.00020679637,0.00037336326,0.00062887155,0.0004777826,0.0021718938],"category_scores_gemma":[0.0004820426,0.00025461454,0.00045421958,0.00034598415,0.000292422,0.00068277615,0.00043929173,0.0004406821,0.0010175538],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025106687,0.00018635663,0.002083596,0.00012465302,0.00006476615,0.00014483825,0.00026175744,0.4639802,0.13391481,0.022000458,0.0019439263,0.3750435],"study_design_scores_gemma":[0.00000748135,0.000022261034,0.000104743376,0.0000026443613,0.0000036859965,0.000027180713,0.000010446709,0.99348253,0.004614899,0.00075984513,0.0009569624,0.0000072699518],"about_ca_topic_score_codex":0.0019688902,"about_ca_topic_score_gemma":0.0026063751,"teacher_disagreement_score":0.0021718938,"about_ca_system_score_codex":0.0002181318,"about_ca_system_score_gemma":0.00050085096,"threshold_uncertainty_score":0.0072657466},"labels":[],"label_agreement":null},{"id":"W4404198737","doi":"10.1029/2024jb029046","title":"Conformably Variable Geocentric Axial Dipole at ca. 2.1 Ga: Paleomagnetic Dispersion of the Indin Dyke Swarm, Slave Craton","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Commission Géologique du Canada; Chinese Academy of Sciences; National Natural Science Foundation of China","keywords":"Paleomagnetism; Craton; Swarm behaviour; Geology; Dipole; Geophysics; Dispersion (optics); Variable (mathematics); Geodesy; Physics; Geometry; Seismology; Mathematics; Optics; Mathematical analysis; Quantum mechanics; Mathematical optimization","score_opus":0.013711865619884231,"score_gpt":0.2913505154390501,"score_spread":0.27763864981916586,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404198737","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99895084,0.000026479049,0.00016527926,0.000008328904,0.0000010499257,0.000002322242,0.00014264317,0.0000067780447,0.0006961726],"genre_scores_gemma":[0.99952793,0.000012475896,0.00013243586,0.0000043695104,0.0000011873885,0.000002597215,0.0002191647,0.000005114881,0.00009467906],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989057,0.000011632234,0.0000054909747,0.00005141926,0.000020854843,0.000020008336],"domain_scores_gemma":[0.9997198,0.000047018224,0.00006499098,0.00005611139,0.00007048914,0.00004167328],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002718193,0.00018653482,0.0002902627,0.0009069632,0.0005916909,0.00061668997,0.00033417408,0.0002038724,0.0007549631],"category_scores_gemma":[0.0009287794,0.00017008878,0.00016226924,0.0008469292,0.0005890673,0.00016442752,0.0006002374,0.00024917955,0.00014125193],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015915128,0.000016417644,0.9748377,0.000015502388,0.000058896145,0.00022906117,0.0011279706,0.0014879021,0.017219078,0.00020390401,0.00017193725,0.0044724313],"study_design_scores_gemma":[0.0000039307565,0.0000085338725,0.9984653,0.000002429814,0.0000058864657,0.00007635578,0.00021141015,0.0006770381,0.00026322866,0.00002705598,0.0002564071,0.0000024875753],"about_ca_topic_score_codex":0.04536329,"about_ca_topic_score_gemma":0.08018632,"teacher_disagreement_score":0.04536329,"about_ca_system_score_codex":0.00076120975,"about_ca_system_score_gemma":0.0003340903,"threshold_uncertainty_score":0.09019846},"labels":[],"label_agreement":null},{"id":"W4404424955","doi":"10.1029/2024jb029506","title":"Brittle Regime Slip Partitioned Damage and Deformation Mechanisms Along the Eastern Denali Fault Zone in Southwestern Yukon","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey","keywords":"Geology; Brittleness; Slip (aerodynamics); Seismology; Deformation (meteorology); Geotechnical engineering; Materials science; Engineering; Composite material","score_opus":0.03945882148677169,"score_gpt":0.30474166530980784,"score_spread":0.26528284382303613,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404424955","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996743,0.00003951814,0.000023347187,0.000004097292,2.5761042e-7,0.0000017774559,0.000102344704,0.0000026621365,0.00015166547],"genre_scores_gemma":[0.9994825,0.000037997004,0.00004997695,0.000003341153,2.2655273e-7,0.0000023701928,0.00026150738,6.712581e-7,0.00016142837],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999105,0.000005398761,0.000009230842,0.000026237729,0.000017111523,0.000031484615],"domain_scores_gemma":[0.9998621,0.000010966217,0.000041821953,0.000012052605,0.000048121212,0.000024881245],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000092327144,0.00019177311,0.00021869742,0.00093564333,0.0004844423,0.000377377,0.00029690727,0.00020958173,0.00055235653],"category_scores_gemma":[0.0001644871,0.0001586751,0.00012310523,0.0010381835,0.0003119162,0.00020250908,0.00036664846,0.00007813867,0.0000680382],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004905285,0.000014227991,0.98195165,0.000040832452,0.00005040462,0.0002907376,0.0007985143,0.0004927032,0.00969077,0.00009269025,0.00008122052,0.006447132],"study_design_scores_gemma":[0.0000011484226,0.000006869434,0.99904007,0.0000031103307,0.000005762877,0.000043128486,0.00040797127,0.00020323349,0.00013991419,0.000008532841,0.00013849938,0.0000016721515],"about_ca_topic_score_codex":0.2520039,"about_ca_topic_score_gemma":0.55058396,"teacher_disagreement_score":0.7479961,"about_ca_system_score_codex":0.0011435698,"about_ca_system_score_gemma":0.0009421046,"threshold_uncertainty_score":0.5010742},"labels":[],"label_agreement":null},{"id":"W4405002741","doi":"10.1029/2024jb029013","title":"Quantifying Crustal Growth in Arc‐Backarc Systems: Gravity Inversion Modeling of the Lau Basin","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa; Mount Allison University; Memorial University of Newfoundland","funders":"Alliance de recherche numérique du Canada; Canada First Research Excellence Fund; Natural Sciences and Engineering Research Council of Canada; Government of Canada","keywords":"Geology; Seafloor spreading; Volcano; Crust; Structural basin; Inversion (geology); Island arc; Volcanic arc; Mantle (geology); Back-arc basin; Subduction; Volcanism; Arc (geometry); Accretion (finance); Geophysics; Seismology; Tectonics; Geomorphology; Geometry","score_opus":0.0750743340475583,"score_gpt":0.3144174868837697,"score_spread":0.23934315283621138,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405002741","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9940707,0.000034983088,0.004495187,0.00006304912,0.000002509939,0.000009118271,0.00013988273,0.00011170028,0.0010728172],"genre_scores_gemma":[0.99769884,0.000022640806,0.0019265224,0.000005824374,0.000001702526,0.000008080345,0.00009298341,0.000014482392,0.00022892827],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99994874,0.000014799966,0.0000024056083,0.000014486991,0.000008642398,0.0000108746],"domain_scores_gemma":[0.9998472,0.0000768651,0.000017377502,0.000016157175,0.000022627455,0.000019705923],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019710645,0.0004557988,0.0003460073,0.00048996264,0.0003576993,0.0007008734,0.00058596453,0.00057543186,0.0007561204],"category_scores_gemma":[0.0007178067,0.0003484765,0.00052473263,0.00040672894,0.0004651082,0.00039123534,0.00046065068,0.00046364852,0.000081162056],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023610615,0.000026601983,0.010222238,0.0000058186283,0.000020667818,0.00004333063,0.00003119715,0.9858807,0.0011961417,0.00021215131,0.00005829084,0.0022794174],"study_design_scores_gemma":[0.0000029953615,0.0000038116357,0.0016771399,7.4537127e-7,0.0000019740553,0.00000291725,0.000007616881,0.9981109,0.000102277656,0.00005390769,0.000033735567,0.0000019467186],"about_ca_topic_score_codex":0.09824639,"about_ca_topic_score_gemma":0.05001851,"teacher_disagreement_score":0.09824639,"about_ca_system_score_codex":0.00090054446,"about_ca_system_score_gemma":0.0009940668,"threshold_uncertainty_score":0.1953491},"labels":[],"label_agreement":null},{"id":"W4405128068","doi":"10.1029/2024jb029914","title":"Manganese Cycling Driven by Fluctuating Redox Chemocline in the Ediacaran Ocean","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"National Natural Science Foundation of China","keywords":"Chemocline; Cycling; Manganese; Redox; Geology; Oceanography; Chemistry; Inorganic chemistry; Geography; Water column","score_opus":0.023138161208597068,"score_gpt":0.32381158792680576,"score_spread":0.3006734267182087,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405128068","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989028,0.00037314944,0.00011927715,0.00004111892,0.0000047177323,0.0000015811996,0.00017798331,0.0000090744525,0.00037037872],"genre_scores_gemma":[0.9994641,0.00017041809,0.00009407503,0.0000178564,0.0000046960736,0.000001954619,0.0001444843,0.0000024532412,0.00010008946],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999291,0.000004939582,0.0000055258374,0.000034565353,0.000009707465,0.000016250418],"domain_scores_gemma":[0.9999417,0.00000510714,0.000021360267,0.000003236299,0.000015872725,0.000012722047],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001661232,0.00036037748,0.0002873339,0.0006519657,0.0003626988,0.000457356,0.00026000393,0.00023337515,0.0004059488],"category_scores_gemma":[0.00015203274,0.00020927122,0.00013937349,0.00074898027,0.0002647783,0.00023256596,0.0005801586,0.00016974514,0.00005084806],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002200275,0.00002805939,0.8347848,0.00012926882,0.00019021574,0.00060561055,0.0009995033,0.0011417642,0.14953896,0.00032625961,0.00026095743,0.011774506],"study_design_scores_gemma":[0.00000772785,0.000018516572,0.9959215,0.0000063747434,0.000030804425,0.00005467565,0.00033642986,0.00064682745,0.0021399483,0.00009429589,0.00073693687,0.0000059929394],"about_ca_topic_score_codex":0.012212871,"about_ca_topic_score_gemma":0.013609187,"teacher_disagreement_score":0.012212871,"about_ca_system_score_codex":0.00051434635,"about_ca_system_score_gemma":0.00026794354,"threshold_uncertainty_score":0.024283588},"labels":[],"label_agreement":null},{"id":"W4405695520","doi":"10.1029/2024jb030063","title":"Ferrous Iron (Fe<sup>+2</sup>) Released From Iron‐Rich Chlorite as a Reductant for Unconformity‐Related Uranium Mineralization: Insights From Reactive Fluid Flow Modeling","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Radioactive element chemistry and processing","field":"Chemistry","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Windsor","funders":"National Key Research and Development Program of China; China University of Geosciences; Ministry of Human Resources and Social Security; National Natural Science Foundation of China","keywords":"Uranium; Ferrous; Mineralization (soil science); Chemistry; Chlorite; Unconformity; Radiochemistry; Geology; Geochemistry; Metallurgy; Materials science; Quartz; Sedimentary rock","score_opus":0.03052671410228183,"score_gpt":0.3221580860620022,"score_spread":0.2916313719597204,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405695520","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98509073,0.0001319325,0.012754458,0.00011090933,0.000010352285,0.000015648293,0.00011742849,0.00007706666,0.001691568],"genre_scores_gemma":[0.9971185,0.00008311625,0.0023604885,0.000009590943,0.0000015234266,0.000008076877,0.000051528234,0.000006075445,0.00036111183],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99995625,0.0000116076,0.0000027498675,0.000008528418,0.0000116334095,0.000009155985],"domain_scores_gemma":[0.99988484,0.000066800065,0.000020558242,0.00000496064,0.000016323958,0.0000065221125],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018724296,0.00031576338,0.00020319765,0.00021854357,0.0001442955,0.00027578638,0.0002789063,0.00042849654,0.00055010803],"category_scores_gemma":[0.00031083266,0.00012220058,0.00037639381,0.000099230674,0.00020970627,0.00025679433,0.00017421893,0.00021303781,0.000065724664],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024136563,0.00012378443,0.009163129,0.00014853707,0.000042165368,0.00021695465,0.00006396107,0.68350625,0.296376,0.0018885974,0.00020240668,0.008026948],"study_design_scores_gemma":[0.000008345425,0.000045943638,0.0007487764,0.0000019636734,0.0000064366604,0.000011473406,0.000016803278,0.95739895,0.04140218,0.00019568893,0.0001583281,0.0000051259426],"about_ca_topic_score_codex":0.0057734763,"about_ca_topic_score_gemma":0.0027918958,"teacher_disagreement_score":0.0057734763,"about_ca_system_score_codex":0.00039223055,"about_ca_system_score_gemma":0.00024836385,"threshold_uncertainty_score":0.011479735},"labels":[],"label_agreement":null},{"id":"W4406795869","doi":"10.1029/2024jb029569","title":"Evidence for Magma‐Rich and Magma‐Poor Characteristics Across the Continent‐Ocean Transition Offshore Central Nova Scotia as Deduced From <i>V</i><sub><i>p</i></sub>/<i>V</i><sub><i>s</i></sub> Ratios Using 4‐Component Seismic Data","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geophysical Studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Nova Scotia Department of Energy and Mines; Offshore Energy Research Association","keywords":"Nova scotia; Magma; Geology; Nova (rocket); Submarine pipeline; Geochemistry; Oceanography; Volcano","score_opus":0.08707436818236056,"score_gpt":0.3412747837773596,"score_spread":0.25420041559499906,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406795869","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987379,0.00003834401,0.00006659527,0.00001230306,0.0000011457552,0.000003747365,0.00033982057,0.0000063612924,0.0007937626],"genre_scores_gemma":[0.99960285,0.000018817513,0.000048253478,0.0000050835956,4.0652762e-7,0.0000013881429,0.00020071362,0.0000014887005,0.00012105671],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999052,0.000006926301,0.000008006907,0.00002587226,0.000020735208,0.00003328371],"domain_scores_gemma":[0.9995408,0.000046462657,0.00011380004,0.000036107554,0.00014462663,0.0001182151],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015298159,0.0002505902,0.00014877676,0.0011249043,0.0003517463,0.0007049889,0.00026661434,0.00016467918,0.000854062],"category_scores_gemma":[0.00050130015,0.00022337121,0.00021484533,0.0008538858,0.0005180553,0.00013213593,0.0004701342,0.00013940738,0.00014943062],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008348424,0.0000071601353,0.9877479,0.000014894027,0.00003893531,0.0001840396,0.000202343,0.001028561,0.008628907,0.0000710643,0.00009957226,0.001893176],"study_design_scores_gemma":[0.0000022517447,0.0000041971716,0.99895155,0.0000036204729,0.000005205105,0.000023729595,0.0001613634,0.0005944797,0.00017791682,0.0000064203523,0.00006729726,0.0000018603638],"about_ca_topic_score_codex":0.69493973,"about_ca_topic_score_gemma":0.7745349,"teacher_disagreement_score":0.30506027,"about_ca_system_score_codex":0.0015334002,"about_ca_system_score_gemma":0.0013497993,"threshold_uncertainty_score":0.6137136},"labels":[],"label_agreement":null},{"id":"W4406916531","doi":"10.1029/2024jb030213","title":"Alteration's Control on Frictional Behavior and the Depth of the Ductile Shear Zone in Geothermal Reservoirs in Volcanic Arcs","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"European Research Council","keywords":"Shear zone; Geology; Geothermal gradient; Volcano; Shear (geology); Petrology; Geotechnical engineering; Seismology; Tectonics; Paleontology","score_opus":0.017864841676313775,"score_gpt":0.294906595479753,"score_spread":0.2770417538034392,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406916531","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9998091,0.00003213971,0.000036670375,0.000002254628,1.9117549e-7,0.0000010971917,0.00001860155,0.0000021266917,0.000097706565],"genre_scores_gemma":[0.9998865,0.000013587129,0.000026805914,7.3524694e-7,1.6475474e-7,8.329621e-7,0.000015578344,6.782456e-7,0.00005502142],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.999928,0.000010614368,0.000007807728,0.000015476191,0.000018948576,0.000019130477],"domain_scores_gemma":[0.99984276,0.000028382548,0.0000590265,0.0000100460475,0.000030661733,0.000029161443],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000111872316,0.00013241456,0.00015214397,0.00028183463,0.00019071458,0.00034583578,0.00016298797,0.00014902948,0.00060438726],"category_scores_gemma":[0.0002877602,0.00016429351,0.000088648834,0.00025761314,0.0003095433,0.00022742533,0.0002149453,0.00015461704,0.00005713161],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005171415,0.000040224506,0.04883561,0.000074201685,0.000025715977,0.00019166517,0.0003016248,0.0008518042,0.9466036,0.000067379304,0.000019098068,0.002471999],"study_design_scores_gemma":[0.000010923856,0.00031405728,0.6875089,0.000009564134,0.000024109328,0.00020123851,0.00065871526,0.002467711,0.3080735,0.00005433266,0.000664844,0.0000122320025],"about_ca_topic_score_codex":0.0023006815,"about_ca_topic_score_gemma":0.0033132443,"teacher_disagreement_score":0.0023006815,"about_ca_system_score_codex":0.00024466493,"about_ca_system_score_gemma":0.000119773424,"threshold_uncertainty_score":0.004574597},"labels":[],"label_agreement":null},{"id":"W4407314440","doi":"10.1029/2024jb028929","title":"Integrating Gravity, Magnetic, and Magnetotelluric Data Over Devon Ice Cap, Canadian Arctic, to Investigate the Subglacial Geology","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Yukon University; University of Alberta; University of Waterloo","funders":"Weston Family Foundation; G. Unger Vetlesen Foundation","keywords":"Magnetotellurics; Geology; Ice caps; The arctic; Arctic; Geophysics; Oceanography; Geomorphology; Glacier; Engineering; Electrical resistivity and conductivity","score_opus":0.023881638859157672,"score_gpt":0.3162939466823106,"score_spread":0.2924123078231529,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407314440","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9945528,0.00043219607,0.00031089893,0.00006788445,0.000011371873,0.000019332128,0.0027168288,0.000047271642,0.0018413031],"genre_scores_gemma":[0.9946008,0.000367387,0.0010650088,0.00003415977,0.000009871951,0.000010697053,0.0032250793,0.000010604459,0.00067650864],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99978155,0.000008707836,0.0000071606096,0.000041439525,0.00008124964,0.00007989004],"domain_scores_gemma":[0.9996099,0.000012436423,0.00003141547,0.0000105625695,0.00026295448,0.00007267386],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003141581,0.0008053024,0.00041511035,0.002479763,0.001485917,0.001069408,0.00046893494,0.0003180814,0.0006073447],"category_scores_gemma":[0.0004226408,0.00024139338,0.00044292342,0.003390014,0.00035334594,0.00029585866,0.0005978958,0.00027764053,0.00012827737],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020217222,0.000084109706,0.9460318,0.00010926705,0.00040729134,0.00028490357,0.00070260675,0.009198761,0.013987843,0.00016791206,0.0018586757,0.02696464],"study_design_scores_gemma":[0.000007954678,0.000011701388,0.99265563,0.000014386915,0.000058507325,0.000020000653,0.0004606964,0.0044523105,0.00062269595,0.000020359721,0.0016613287,0.000014498534],"about_ca_topic_score_codex":0.9816372,"about_ca_topic_score_gemma":0.993145,"teacher_disagreement_score":0.01836282,"about_ca_system_score_codex":0.007414249,"about_ca_system_score_gemma":0.009679395,"threshold_uncertainty_score":0.053794384},"labels":[],"label_agreement":null},{"id":"W4407865559","doi":"10.1029/2024jb029476","title":"The Role of the Three‐Dimensional Geometry of Fault Steps on Event Migration During Fluid‐Induced Seismic Sequences","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Horizon 2020 Framework Programme; European Regional Development Fund; Science Foundation Ireland; European Commission; Microseismic Industry Consortium","keywords":"Geology; Geometry; Event (particle physics); Fault (geology); Seismology; Normal fault; Mathematics; Physics","score_opus":0.024167909217441164,"score_gpt":0.30314791263125873,"score_spread":0.27898000341381757,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407865559","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987984,0.000023592587,0.0008021521,0.0000061596725,0.0000011584967,0.0000024116907,0.00006981571,0.000018589606,0.00027780613],"genre_scores_gemma":[0.99968946,0.000010578845,0.00020243796,8.7260406e-7,7.596195e-7,8.1537104e-7,0.00005959122,0.0000037182122,0.000031827873],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998802,0.000025817608,0.000010687878,0.00003903506,0.00001983562,0.000024369649],"domain_scores_gemma":[0.9993637,0.00020887045,0.00023189165,0.000060172242,0.000058681122,0.00007670318],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017259641,0.00020183998,0.0002117254,0.0009069554,0.00019227313,0.0008329263,0.000186667,0.000182356,0.00085508305],"category_scores_gemma":[0.0015368646,0.00015587902,0.0001537171,0.00053429726,0.0003947308,0.00047958357,0.00037982897,0.00012342424,0.00018118853],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00054768065,0.000114949755,0.8053508,0.00010047719,0.00015042187,0.00042608893,0.00092469214,0.0374689,0.12225031,0.001074061,0.00025811754,0.03133342],"study_design_scores_gemma":[0.000004879206,0.000047132107,0.97002923,0.000008522887,0.000021757976,0.00008771074,0.00031631187,0.025613181,0.0033189072,0.0002736475,0.0002615741,0.000017178685],"about_ca_topic_score_codex":0.0029389495,"about_ca_topic_score_gemma":0.0036960628,"teacher_disagreement_score":0.0029389495,"about_ca_system_score_codex":0.00022580549,"about_ca_system_score_gemma":0.00018778005,"threshold_uncertainty_score":0.005843699},"labels":[],"label_agreement":null},{"id":"W4408381159","doi":"10.1029/2024jb030275","title":"3D Shear‐Wave Velocity and Density Modeling of the Northern Cascadia Subduction Zone","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"","keywords":"Subduction; Geology; Seismology; Shear (geology); Wave velocity; Episodic tremor and slip; Geophysics; Petrology; Tectonics","score_opus":0.034439646962887795,"score_gpt":0.29007980880769973,"score_spread":0.2556401618448119,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408381159","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9602062,0.00015428243,0.030725935,0.00029059354,0.000031548097,0.00004805622,0.0011322628,0.00079315726,0.006617901],"genre_scores_gemma":[0.99540114,0.00006314218,0.0032068614,0.000013730095,0.0000049296764,0.000025429861,0.00035228257,0.000035078752,0.00089734315],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999151,0.000016254251,0.0000059873773,0.000026603931,0.000019174942,0.000016822325],"domain_scores_gemma":[0.99982244,0.00004580227,0.00002964485,0.000023735181,0.000042766984,0.000035564663],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021950777,0.00083236257,0.000355875,0.0007248893,0.0004972474,0.0009536867,0.0009766355,0.0009097643,0.0013952],"category_scores_gemma":[0.0008079261,0.0006134897,0.00086442335,0.0005202221,0.000537461,0.00028756028,0.00067563483,0.0004340273,0.00025427275],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014384385,0.000012867363,0.0064857,0.0000064571345,0.000016807575,0.00004566159,0.000035824847,0.99155784,0.00055776845,0.00022490002,0.00010383005,0.0009379579],"study_design_scores_gemma":[0.0000058591318,0.0000037543814,0.002087059,0.0000017323856,0.0000033612873,0.000004729938,0.000011301035,0.99760455,0.00006423755,0.00008392207,0.00012544388,0.0000040674413],"about_ca_topic_score_codex":0.20583268,"about_ca_topic_score_gemma":0.09110016,"teacher_disagreement_score":0.20583268,"about_ca_system_score_codex":0.0016456601,"about_ca_system_score_gemma":0.0015105464,"threshold_uncertainty_score":0.40926915},"labels":[],"label_agreement":null},{"id":"W4408381834","doi":"10.1029/2024jb029295","title":"Unified Nonlinear Elasto‐Visco‐Plastic Rheology for Bituminous Rocks at Variable Pressure and Temperature","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Drilling and Well Engineering","field":"Engineering","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Rheology; Materials science; Nonlinear system; Variable (mathematics); Viscoelasticity; Geotechnical engineering; Composite material; Mechanics; Geology; Mathematics; Physics; Mathematical analysis","score_opus":0.010457869936165176,"score_gpt":0.2783127112190847,"score_spread":0.26785484128291953,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408381834","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6167909,0.0010849531,0.3728973,0.00019852325,0.000058887705,0.00007947411,0.00030485625,0.00033436692,0.008250811],"genre_scores_gemma":[0.99073946,0.00030531036,0.0063042766,0.000013708177,0.000015158453,0.00003546037,0.00010439074,0.000033268567,0.0024490498],"study_design_codex":"simulation_or_modeling","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99990153,0.000019949775,0.0000065300196,0.000019964067,0.00003993562,0.0000120756185],"domain_scores_gemma":[0.9998957,0.00001950971,0.00002733244,0.000023912644,0.000025031164,0.000008535216],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017871415,0.0004987376,0.00047246992,0.00055405486,0.00021002782,0.0005282709,0.00047510103,0.0004325925,0.00066853984],"category_scores_gemma":[0.00039958983,0.00022108434,0.00040186243,0.0002777009,0.00053818995,0.00083306036,0.00044157525,0.00046488945,0.00026592586],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000119838325,0.00013297457,0.0049749827,0.00016054195,0.000057154622,0.0005278038,0.0002146635,0.6158815,0.30903286,0.051292308,0.00058442727,0.017020904],"study_design_scores_gemma":[0.0000054865795,0.000020699166,0.001300827,0.000003991549,0.000003247462,0.00004517997,0.000009363073,0.99180686,0.004086186,0.0023340157,0.00037247612,0.00001174779],"about_ca_topic_score_codex":0.0012756287,"about_ca_topic_score_gemma":0.0008222187,"teacher_disagreement_score":0.0012756287,"about_ca_system_score_codex":0.00039327424,"about_ca_system_score_gemma":0.0003125616,"threshold_uncertainty_score":0.0028533936},"labels":[],"label_agreement":null},{"id":"W4408456718","doi":"10.1029/2024jb030903","title":"On Dislocation Modeling of Megathrust Tsunami Sources","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; University of Victoria","funders":"Fondo Nacional de Desarrollo Científico y Tecnológico","keywords":"Dislocation; Seismology; Geology; Materials science; Composite material","score_opus":0.04435415420441634,"score_gpt":0.33545435924199496,"score_spread":0.2911002050375786,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408456718","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.69859725,0.0005742222,0.2918208,0.00038913317,0.000058915808,0.00005920125,0.0003538176,0.00055975374,0.0075869435],"genre_scores_gemma":[0.99086654,0.00016963166,0.007380451,0.000016727952,0.000005731925,0.000014437912,0.000088993314,0.000032648637,0.0014247542],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989545,0.000034972254,0.00000894133,0.000016586595,0.000027561207,0.000016450296],"domain_scores_gemma":[0.99972266,0.000106443455,0.000043878917,0.000032198008,0.000072934796,0.000021845848],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025052548,0.0004734094,0.0004754034,0.00066258595,0.0002514338,0.0008691293,0.0007507138,0.00083549303,0.0010701774],"category_scores_gemma":[0.0010348058,0.00023645053,0.00048621395,0.00052846957,0.00040158667,0.00047591035,0.00036754433,0.00033595765,0.00024235295],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011389771,0.000019888206,0.0012670277,0.000009344699,0.000008188768,0.000038338556,0.00002381351,0.99407494,0.00088934164,0.0011426099,0.00005965151,0.0024555204],"study_design_scores_gemma":[8.2650035e-7,0.0000035887879,0.00011799653,0.0000013584257,8.965529e-7,0.000003746469,0.000005119815,0.999466,0.00013555308,0.00018602272,0.000077775105,0.0000011781402],"about_ca_topic_score_codex":0.016678322,"about_ca_topic_score_gemma":0.009949914,"teacher_disagreement_score":0.016678322,"about_ca_system_score_codex":0.00097343896,"about_ca_system_score_gemma":0.0007321998,"threshold_uncertainty_score":0.033162534},"labels":[],"label_agreement":null},{"id":"W4408752082","doi":"10.1029/2024jb028839","title":"Trans‐Crustal Geophysical Responses Beneath the Supergiant Timmins‐Porcupine Orogenic Gold Camp, Canada","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Manitoba; Laurentian University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Porcupine; Supergiant; Geophysics; Paleontology; Astronomy; Stars; Physics","score_opus":0.029280136533358727,"score_gpt":0.3187733415491579,"score_spread":0.28949320501579917,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408752082","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960884,0.000048325586,0.00004619213,0.000033806034,0.0000012274431,0.0000057281295,0.00040603537,0.000011417631,0.0033590307],"genre_scores_gemma":[0.9984938,0.00004737458,0.00006561971,0.000009104623,7.547044e-7,0.0000023862872,0.00022621613,0.0000031382624,0.0011516685],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999062,0.0000034701643,0.0000023598816,0.000018190756,0.000028035554,0.00004170383],"domain_scores_gemma":[0.99985456,0.000005960353,0.0000158295,0.000004387544,0.00008964619,0.000029542281],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007281162,0.00025699983,0.00014618602,0.0008599168,0.00071569264,0.0006447247,0.0003750737,0.00017966138,0.0023298187],"category_scores_gemma":[0.00036324657,0.00012198367,0.000113364025,0.0009611048,0.00035261537,0.00018128357,0.0005206155,0.00015663875,0.00021182315],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002888238,0.00003609211,0.91779053,0.00010179107,0.000099036646,0.0012147162,0.006371527,0.0018734914,0.03405796,0.0004836427,0.0014854776,0.036196884],"study_design_scores_gemma":[0.0000033424947,0.000009259338,0.99596477,0.000010656559,0.000007746248,0.000053261763,0.0018900799,0.00050589046,0.00038825255,0.000017855962,0.0011444436,0.000004506826],"about_ca_topic_score_codex":0.9387875,"about_ca_topic_score_gemma":0.97469836,"teacher_disagreement_score":0.06121248,"about_ca_system_score_codex":0.0048552654,"about_ca_system_score_gemma":0.0027183597,"threshold_uncertainty_score":0.12314588},"labels":[],"label_agreement":null},{"id":"W4409159611","doi":"10.1029/2024jb030603","title":"Storms, Sea Ice, and Microseismic Noise in Alaska","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey; National Science Foundation","keywords":"Microseism; Storm; Geology; Oceanography; Winter storm; Noise (video); Seismology; Meteorology; Climatology; Environmental science; Geography; Computer science","score_opus":0.019768103578310246,"score_gpt":0.31260259378846217,"score_spread":0.2928344902101519,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409159611","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993911,0.000033901342,0.000056923756,0.000006838741,0.0000012228303,8.609037e-7,0.00025789492,0.0000014646504,0.00024998395],"genre_scores_gemma":[0.9994562,0.000041339455,0.000055610173,0.000002025987,0.0000017668477,0.0000012866332,0.00029685092,6.653864e-7,0.00014431501],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991894,0.00000978577,0.000009544745,0.000021676791,0.000024939412,0.000015086785],"domain_scores_gemma":[0.99955016,0.00008789189,0.00013664717,0.00002171352,0.00013577513,0.000067819594],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020851278,0.0001325706,0.00013820438,0.0006646512,0.0002860727,0.0004013643,0.00012353268,0.0001131518,0.000525797],"category_scores_gemma":[0.00085821917,0.00008507949,0.00009469377,0.000986644,0.00018314259,0.00017589009,0.0003407547,0.00008931262,0.00007992123],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000031921176,0.000007449882,0.99621326,0.0000053983013,0.00001756885,0.00003762382,0.00019846839,0.00077041495,0.00045046484,0.000024790847,0.000056207242,0.0021864788],"study_design_scores_gemma":[6.048194e-7,0.000007297856,0.9989197,0.000003057049,0.0000045054785,0.000015010702,0.00032289306,0.0005130393,0.00006536247,0.0000183982,0.00012857193,0.0000014913851],"about_ca_topic_score_codex":0.25697723,"about_ca_topic_score_gemma":0.34220627,"teacher_disagreement_score":0.25697723,"about_ca_system_score_codex":0.0005649032,"about_ca_system_score_gemma":0.00058530085,"threshold_uncertainty_score":0.5109629},"labels":[],"label_agreement":null},{"id":"W4409325425","doi":"10.1029/2024jb029955","title":"Investigation of Submarine Permafrost Conditions in the Canadian Beaufort Sea Using Diving Wave Tomography","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Polytechnique Montréal; Geological Survey of Canada","funders":"Deutsche Forschungsgemeinschaft","keywords":"Beaufort sea; Permafrost; Submarine; Oceanography; Geology; Beaufort scale; Environmental science; Arctic","score_opus":0.10751088989003553,"score_gpt":0.343976792730895,"score_spread":0.23646590284085944,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409325425","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954867,0.000120053504,0.00067340455,0.000056172135,0.000004656237,0.000013197974,0.0014364558,0.00006907044,0.0021403262],"genre_scores_gemma":[0.9975834,0.000063953914,0.0010083746,0.000012101237,0.0000023233133,0.0000041386306,0.0008891167,0.000009169939,0.00042734394],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998235,0.0000061057935,0.000004804876,0.000029168807,0.00006804685,0.00006838664],"domain_scores_gemma":[0.99967444,0.000026488882,0.000044617387,0.00001954621,0.00018060861,0.00005425626],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014380252,0.0005210479,0.00022812028,0.0017665857,0.0010733063,0.0007834537,0.00061011617,0.00034852335,0.0010891525],"category_scores_gemma":[0.00042415477,0.0002144851,0.0002799426,0.002174485,0.00040027418,0.0002688968,0.00039935604,0.00025333263,0.00015056267],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016195294,0.00010609693,0.87679076,0.00007141199,0.00016557184,0.00068723375,0.00092540664,0.018155897,0.045451615,0.00045112244,0.0018847127,0.055148173],"study_design_scores_gemma":[0.000005373756,0.000009129183,0.9793584,0.000008311455,0.000017544846,0.000060532697,0.0004470556,0.017432163,0.001281418,0.000025550082,0.0013361489,0.000018366687],"about_ca_topic_score_codex":0.9572275,"about_ca_topic_score_gemma":0.98278886,"teacher_disagreement_score":0.042772472,"about_ca_system_score_codex":0.0034835138,"about_ca_system_score_gemma":0.005539529,"threshold_uncertainty_score":0.08604866},"labels":[],"label_agreement":null},{"id":"W4409365697","doi":"10.1029/2024jb030204","title":"Modelling Partial Melting in Sinking Greenstone Belts With Implications for Archaean Continental Crust Formation","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"State Key Laboratory of Lithospheric Evolution; National Natural Science Foundation of China","keywords":"Archean; Greenstone belt; Continental crust; Geology; Geochemistry; Partial melting; Crust; Earth science; Petrology","score_opus":0.05454042606746372,"score_gpt":0.32446999948186894,"score_spread":0.2699295734144052,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409365697","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99691546,0.000048411122,0.00088553486,0.000061674546,0.0000056341855,0.000016504515,0.00042309138,0.000052652165,0.0015910398],"genre_scores_gemma":[0.9981536,0.00003919202,0.0011340214,0.000013354622,0.000002907906,0.000015320746,0.00021740094,0.000026145484,0.0003980442],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999076,0.000021098738,0.0000063215502,0.000025366098,0.000011599046,0.000028033188],"domain_scores_gemma":[0.99975675,0.000107313674,0.000026958942,0.000037923288,0.000032516888,0.000038592818],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031838784,0.00066018,0.00046623035,0.00080532354,0.0005925086,0.0014469582,0.0011742411,0.001968317,0.0031780377],"category_scores_gemma":[0.00091205514,0.0006864599,0.0011616732,0.0008865163,0.0006728794,0.00048820907,0.0006301579,0.00050535804,0.00035233566],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011253511,0.00007658888,0.029568445,0.000040188508,0.00009168902,0.00020927507,0.000090983216,0.96402466,0.0032368226,0.00044770652,0.00011070233,0.0019904247],"study_design_scores_gemma":[0.00005036615,0.00004278937,0.014961117,0.000009928216,0.000027025058,0.000037276055,0.00011736386,0.98329306,0.0006777529,0.00031607386,0.00045049973,0.000016717404],"about_ca_topic_score_codex":0.077938326,"about_ca_topic_score_gemma":0.049101356,"teacher_disagreement_score":0.077938326,"about_ca_system_score_codex":0.002099752,"about_ca_system_score_gemma":0.0011186576,"threshold_uncertainty_score":0.15496933},"labels":[],"label_agreement":null},{"id":"W4409466031","doi":"10.1029/2024jb030928","title":"Is the Geodynamo Characterized by a Distinct Geomagnetic Secular Variation Regime During the Cretaceous Normal Superchron?","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Russian Science Foundation; Deutsche Forschungsgemeinschaft","keywords":"Secular variation; Earth's magnetic field; Dynamo theory; Geology; Variation (astronomy); Geophysics; Geomagnetic secular variation; Cretaceous; Paleontology; Geomagnetic reversal; Dynamo; Magnetic field; Physics; Astronomy; Geomagnetic storm","score_opus":0.009759581518016265,"score_gpt":0.2850966735265283,"score_spread":0.27533709200851203,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409466031","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991553,0.000074868665,0.000081851904,0.000015506173,0.0000015099745,0.0000015641529,0.0001277544,0.0000034189143,0.0005381698],"genre_scores_gemma":[0.99981326,0.000015986772,0.00002362692,0.0000031895522,0.0000019695306,6.19722e-7,0.00009191799,0.000001316466,0.000048163536],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988556,0.000016899992,0.000008902851,0.00004528503,0.000014531391,0.000028797329],"domain_scores_gemma":[0.99966836,0.000044559543,0.00013678786,0.000041739266,0.00006453825,0.00004398097],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023016434,0.00012605463,0.00017587331,0.0009599846,0.00029991413,0.0005814135,0.00018824992,0.00017056058,0.0009831397],"category_scores_gemma":[0.0005190223,0.000086638,0.000112522685,0.00093546556,0.0007832354,0.00023893981,0.00031918322,0.00014052862,0.00013562304],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000089243644,0.000007640714,0.9826104,0.000013344629,0.000049565995,0.00008714739,0.00070959807,0.00022243617,0.011875618,0.00016189598,0.00008414495,0.0040890253],"study_design_scores_gemma":[6.5897933e-7,0.0000029153612,0.9996119,0.000001006383,0.0000022449756,0.000017189996,0.00008759824,0.000094114446,0.000078539844,0.000013462648,0.00008944036,9.769522e-7],"about_ca_topic_score_codex":0.023262816,"about_ca_topic_score_gemma":0.04057741,"teacher_disagreement_score":0.023262816,"about_ca_system_score_codex":0.00041638158,"about_ca_system_score_gemma":0.00027810782,"threshold_uncertainty_score":0.046254873},"labels":[],"label_agreement":null},{"id":"W4409768177","doi":"10.1029/2024jb030654","title":"Subducted Slab Slipping Underneath the Northern Edge of the Pacific Large Low‐Shear‐Velocity Province in D″","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Japan Society for the Promotion of Science; U.S. Geological Survey; Institut de Physique du Globe de Paris; China Earthquake Administration; University of California, Santa Barbara; University of Nevada, Reno; University of Oregon; Natural Resources Canada; University of Washington; National Oceanic and Atmospheric Administration; Universiteit Utrecht; California Institute of Technology","keywords":"Slipping; Slab; Geology; Subduction; Seismology; Shear (geology); Enhanced Data Rates for GSM Evolution; Slab window; Geometry; Petrology; Geophysics; Oceanic crust; Engineering","score_opus":0.028332611472710628,"score_gpt":0.2994384194717878,"score_spread":0.27110580799907713,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409768177","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981445,0.000010090432,0.00057339907,0.000020713127,0.0000024092137,0.0000025601837,0.0002151036,0.00006879176,0.0009623708],"genre_scores_gemma":[0.9987565,0.000007920212,0.00055940106,0.000005048971,7.778737e-7,0.0000017232439,0.0004005083,0.000008114253,0.00025989258],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996936,0.0000017578798,0.0000012741577,0.000008700729,0.0000068183617,0.000012128434],"domain_scores_gemma":[0.9999461,0.0000064571673,0.000008955437,0.000005515912,0.000014954376,0.00001803111],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000052079202,0.00020758915,0.0001370349,0.00045927352,0.00023833211,0.0003979732,0.00025625355,0.00016993721,0.0012199502],"category_scores_gemma":[0.00022850995,0.00019585482,0.00022793809,0.0003735623,0.00018096356,0.00014142712,0.0003304541,0.0002622028,0.00015284687],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007453907,0.00021770953,0.7250411,0.00007412543,0.00019663671,0.0011478906,0.000949989,0.058884766,0.15323885,0.00081300887,0.0014288337,0.057261746],"study_design_scores_gemma":[0.00005838426,0.00006038217,0.778271,0.000015696598,0.00006413522,0.00017749897,0.00067508547,0.20532197,0.013348427,0.00029277572,0.0016801747,0.000034442346],"about_ca_topic_score_codex":0.08003178,"about_ca_topic_score_gemma":0.07978105,"teacher_disagreement_score":0.08003178,"about_ca_system_score_codex":0.0003159564,"about_ca_system_score_gemma":0.0006100449,"threshold_uncertainty_score":0.15913188},"labels":[],"label_agreement":null},{"id":"W4409770818","doi":"10.1029/2024jb030279","title":"Shallow Lingering and Deep Transient Seismicity Related to Hydraulic Fracturing in the Changning Shale Gas Field, Sichuan Basin, China","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Induced seismicity; Shale gas; Hydraulic fracturing; Geology; China; Natural gas field; Oil shale; Structural basin; Sichuan basin; Seismology; Transient (computer programming); Natural gas; Mining engineering; Petroleum engineering; Earth science; Geochemistry; Geomorphology; Paleontology; Engineering; Archaeology; Geography","score_opus":0.01738298633787498,"score_gpt":0.3034238446785667,"score_spread":0.2860408583406917,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409770818","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99956924,0.000021398544,0.00009857948,0.00001970659,0.0000013541603,0.0000027976157,0.00014016689,0.000011269791,0.00013550685],"genre_scores_gemma":[0.9994862,0.000017297154,0.00008083277,0.0000047861495,0.0000028215723,0.0000031074728,0.00028727646,9.987302e-7,0.00011653835],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991953,0.000006994926,0.0000065631584,0.000025556672,0.000015363534,0.000026012016],"domain_scores_gemma":[0.99980825,0.00002328234,0.00004419253,0.00001581923,0.000042428994,0.0000660116],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021024421,0.0003490201,0.00018572694,0.0016390755,0.00041734902,0.000285297,0.00030153635,0.00029576023,0.0004669778],"category_scores_gemma":[0.00027623243,0.00017738636,0.00020314069,0.0012443382,0.00034449846,0.0002707338,0.0004161796,0.00012406164,0.000048807586],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011416663,0.00009986016,0.9542875,0.00007273654,0.000080585436,0.0006560938,0.00071332755,0.015067237,0.010920334,0.00024591768,0.00054990826,0.017192274],"study_design_scores_gemma":[0.0000071677173,0.00002686983,0.9858505,0.000004810407,0.000014091942,0.000031560885,0.00029689466,0.013104312,0.00036726688,0.00006041015,0.0002264548,0.000009625462],"about_ca_topic_score_codex":0.08008478,"about_ca_topic_score_gemma":0.11785955,"teacher_disagreement_score":0.08008478,"about_ca_system_score_codex":0.00062859076,"about_ca_system_score_gemma":0.000899183,"threshold_uncertainty_score":0.15923727},"labels":[],"label_agreement":null},{"id":"W4410111538","doi":"10.1029/2024jb030712","title":"Mapping Crustal Vp/Vs in North America With a Machine Learning Approach","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Artificial intelligence; Computer science","score_opus":0.02244884239106559,"score_gpt":0.28187942337199123,"score_spread":0.25943058098092564,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410111538","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98386,0.0004257668,0.012232044,0.00021627305,0.0000100062125,0.000016071057,0.0012267908,0.00047658163,0.001536494],"genre_scores_gemma":[0.98765904,0.0001226956,0.010499922,0.000016576138,0.000007278106,0.000010149288,0.0012782596,0.000015043081,0.00039100047],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998945,0.000023572258,0.0000056999834,0.00004221103,0.00001838399,0.00001566752],"domain_scores_gemma":[0.9996799,0.00009051617,0.00006470231,0.00003332979,0.0001102035,0.000021307887],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003212509,0.00052270415,0.00022204788,0.0020635752,0.00029230493,0.0005182481,0.00044626836,0.00031575162,0.0006705962],"category_scores_gemma":[0.0009434763,0.00024146843,0.00036384683,0.0022641756,0.00020892352,0.0003776235,0.0004249602,0.00029394875,0.00015880255],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009207606,0.00010261056,0.31952706,0.000060521244,0.00022528935,0.00023909137,0.0002182584,0.47012028,0.00507497,0.00049690215,0.0027240003,0.20111889],"study_design_scores_gemma":[0.00000677232,0.00001287231,0.14840582,0.000016926497,0.000019758681,0.000029830395,0.00019099384,0.84893125,0.00070235605,0.0006506563,0.0010156524,0.000017164415],"about_ca_topic_score_codex":0.2348574,"about_ca_topic_score_gemma":0.25766185,"teacher_disagreement_score":0.7651426,"about_ca_system_score_codex":0.0011328155,"about_ca_system_score_gemma":0.00089651765,"threshold_uncertainty_score":0.4669807},"labels":[],"label_agreement":null},{"id":"W4410147088","doi":"10.1029/2024jb030831","title":"The Heterogeneous Mantle Transition Zone Beneath the Tarim Craton and Adjacent Region: Insight Into the Thermal Processes by the Cenozoic Reactivation","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Craton; Transition zone; Geology; Cenozoic; Mantle (geology); Tarim basin; Geophysics; Paleontology; Tectonics","score_opus":0.01846860517254584,"score_gpt":0.27601716817935407,"score_spread":0.25754856300680823,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410147088","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990369,0.000080013306,0.00026359345,0.000012033084,9.699936e-7,0.0000031825075,0.000082324725,0.000014498953,0.00050651556],"genre_scores_gemma":[0.99960357,0.00003635221,0.00021286389,0.000003978019,0.0000017533047,0.0000016335258,0.000054235294,0.0000027985018,0.00008276886],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999639,0.0000023252958,0.000002062474,0.000011703894,0.000006161617,0.000013805533],"domain_scores_gemma":[0.9999471,0.000008454906,0.00001783854,0.000005067815,0.0000114863515,0.000010110804],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008968199,0.0002736142,0.0001471092,0.0011311425,0.00022321091,0.00043876102,0.0002601626,0.00022539313,0.0011384381],"category_scores_gemma":[0.00019265045,0.0001531033,0.0001374183,0.0007614198,0.0002608198,0.00022828457,0.00046236068,0.00014488159,0.00012860143],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023972533,0.000047988524,0.8175153,0.00007888779,0.000063640095,0.0005238266,0.0012473388,0.0027004927,0.15148163,0.0004003392,0.00011148221,0.025589366],"study_design_scores_gemma":[0.0000045110824,0.000018630972,0.99437296,0.000006934512,0.000017812961,0.00007712402,0.00037553048,0.0034296308,0.0014794049,0.00004489493,0.00016815981,0.000004281745],"about_ca_topic_score_codex":0.016287634,"about_ca_topic_score_gemma":0.021845097,"teacher_disagreement_score":0.016287634,"about_ca_system_score_codex":0.00020733733,"about_ca_system_score_gemma":0.00021849899,"threshold_uncertainty_score":0.032385647},"labels":[],"label_agreement":null},{"id":"W4410505026","doi":"10.1029/2025jb031227","title":"Link Between Enhanced Pore Surface Relaxivity and Mineral Alteration in Basalts","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Fredericton","funders":"","keywords":"Basalt; Mineral; Geology; Geochemistry; Mineralogy; Materials science; Metallurgy","score_opus":0.025699113731175362,"score_gpt":0.33207197204033306,"score_spread":0.3063728583091577,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410505026","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99896216,0.00007604603,0.00052878965,0.000009398929,0.0000013585077,0.000002829152,0.000047355774,0.0000123002965,0.0003597714],"genre_scores_gemma":[0.9995378,0.00002603727,0.00024475492,0.0000051903194,0.0000012047724,0.0000018436402,0.000037491136,0.0000028904021,0.00014279384],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999473,0.0000052903756,0.0000033462313,0.000019611603,0.000013756231,0.000010707154],"domain_scores_gemma":[0.9998103,0.000058278485,0.00005659269,0.0000098650235,0.000041192874,0.000023706614],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010475853,0.000103769074,0.00013433993,0.00040392662,0.0001377317,0.00035978775,0.00010823013,0.00014170102,0.0009537752],"category_scores_gemma":[0.00034767692,0.00013652976,0.000044692024,0.00012507725,0.00027138815,0.00024985088,0.00013206188,0.0001593214,0.0000951321],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005566444,0.000008548296,0.019298853,0.000020572976,0.000009346443,0.000096635194,0.00005105996,0.00006913883,0.9790756,0.00003448001,0.00001543074,0.0012646962],"study_design_scores_gemma":[0.000008017441,0.0001271562,0.6828157,0.000004993525,0.000018076806,0.000669777,0.0002442116,0.0019559774,0.31344372,0.00013240235,0.00057122344,0.00000864667],"about_ca_topic_score_codex":0.0015178156,"about_ca_topic_score_gemma":0.002380914,"teacher_disagreement_score":0.0015178156,"about_ca_system_score_codex":0.0001461045,"about_ca_system_score_gemma":0.00009571245,"threshold_uncertainty_score":0.0031906366},"labels":[],"label_agreement":null},{"id":"W4411310272","doi":"10.1029/2024jb029730","title":"Potential Ice Sheet Modulation of Volcanism in West Antarctica: Constraints on the Cadence and Magnitude of Melt Delivery Into the Crust","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Crust; Cadence; Geology; Volcanism; Magnitude (astronomy); Modulation (music); Antarctic ice sheet; Geophysics; Seismology; Physics; Cryosphere; Astronomy; Climatology; Tectonics","score_opus":0.030810064231916977,"score_gpt":0.30410046332929336,"score_spread":0.2732903990973764,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411310272","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99914193,0.00008447102,0.00007064788,0.000025193305,0.000001089373,0.000001799167,0.00012278827,0.0000044296808,0.0005476858],"genre_scores_gemma":[0.99982077,0.000034744793,0.000030018855,0.0000035481314,0.0000016656819,0.0000014116507,0.000062041436,0.0000016258881,0.000044232926],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995995,0.000010888617,0.0000031710808,0.00000776359,0.000005046471,0.000013134492],"domain_scores_gemma":[0.9997907,0.000063825326,0.000056263165,0.000019966234,0.000024958676,0.00004431359],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019776062,0.00026158607,0.00026137664,0.0005618409,0.00034896753,0.00064113736,0.00027539567,0.00030251362,0.0013719479],"category_scores_gemma":[0.00046948373,0.00017643128,0.0002787202,0.00049063447,0.00030450904,0.00026230759,0.0003149354,0.00012023675,0.00016336716],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010799537,0.00007604423,0.8161733,0.00020063262,0.0002869184,0.0006343988,0.0007304308,0.02412562,0.14429699,0.0008032285,0.0003613771,0.011231221],"study_design_scores_gemma":[0.0000114430795,0.00005159274,0.9882421,0.000007259444,0.000028691484,0.000057184636,0.00017944546,0.009634703,0.0013915322,0.00013610687,0.000250973,0.000008970485],"about_ca_topic_score_codex":0.015155674,"about_ca_topic_score_gemma":0.016731268,"teacher_disagreement_score":0.015155674,"about_ca_system_score_codex":0.0005219867,"about_ca_system_score_gemma":0.00028317107,"threshold_uncertainty_score":0.030134916},"labels":[],"label_agreement":null},{"id":"W4411375653","doi":"10.1029/2024jb030977","title":"Impact of Thermally Induced Cracks on Elastic Modulus Dispersion and Attenuation in Fluid‐Saturated Granite","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Energi Simulation; École Normale Supérieure","keywords":"Attenuation; Dispersion (optics); Materials science; Elastic modulus; Composite material; Modulus; Geology; Geotechnical engineering; Optics; Physics","score_opus":0.029693570834440425,"score_gpt":0.3399503390300254,"score_spread":0.310256768195585,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411375653","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991936,0.00004876451,0.0005560222,0.0000055897185,0.0000010346884,0.000002331711,0.000039397673,0.000017455257,0.00013577357],"genre_scores_gemma":[0.9996517,0.0000148620065,0.00019772515,0.000002104956,2.3191254e-7,0.0000021736455,0.000028275821,0.0000057891452,0.000097256605],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998529,0.0000195979,0.000010470509,0.00003785918,0.000053014996,0.00002607212],"domain_scores_gemma":[0.99973744,0.000097261334,0.000060966657,0.000028321107,0.000051879535,0.000024141553],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016502313,0.00018722333,0.00021377848,0.00026380713,0.00017609028,0.0002882624,0.00019735468,0.00026297945,0.00090096245],"category_scores_gemma":[0.0005259988,0.00017919226,0.00011720667,0.00014473108,0.00045700173,0.00024453687,0.00023638226,0.00029560237,0.00008534895],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001557863,0.000011160425,0.0024733853,0.000031494965,0.000006856873,0.000044933426,0.000049748724,0.0013142208,0.9947247,0.000030657604,0.000009513309,0.0011474486],"study_design_scores_gemma":[0.000009632255,0.00020010136,0.03990242,0.000007804828,0.0000138053865,0.000081227336,0.0001460591,0.0116910655,0.9473319,0.00008952535,0.0005125541,0.000013927537],"about_ca_topic_score_codex":0.0019251478,"about_ca_topic_score_gemma":0.0029614724,"teacher_disagreement_score":0.0019251478,"about_ca_system_score_codex":0.00027688028,"about_ca_system_score_gemma":0.0001503697,"threshold_uncertainty_score":0.0038279295},"labels":[],"label_agreement":null},{"id":"W4413238118","doi":"10.1029/2024jb030976","title":"State of In Situ Stress and Implications for Fault Slip Potential in the Montney Play, Western Canada","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Seismology; Induced seismicity; Borehole; Geomechanics; Fault (geology); Thrust fault; Geotechnical engineering","score_opus":0.028403094553427845,"score_gpt":0.3244767969079105,"score_spread":0.29607370235448266,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413238118","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99821055,0.000037333808,0.000058286652,0.000030417634,8.06358e-7,0.0000041221183,0.00048222588,0.000007688289,0.001168514],"genre_scores_gemma":[0.9992403,0.00003183995,0.000073492665,0.0000055739565,5.451936e-7,0.0000020000693,0.00023728589,0.0000022076952,0.00040682923],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996983,0.000012295504,0.0000111007985,0.000048547136,0.00012102728,0.00010868378],"domain_scores_gemma":[0.99937797,0.000057515237,0.000106717926,0.000025183737,0.00029081572,0.00014179309],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019307873,0.0002794842,0.00023136589,0.0013983427,0.0015887469,0.001238014,0.00084059016,0.0003253521,0.0018757525],"category_scores_gemma":[0.001087991,0.00018466584,0.00020272778,0.0018685439,0.001110853,0.00030586493,0.0005915679,0.00024154555,0.00016366932],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001240506,0.00003184665,0.9844342,0.000023576176,0.00005121164,0.00043960553,0.0011179834,0.003519824,0.0036712224,0.00026418664,0.00038784675,0.005934406],"study_design_scores_gemma":[0.0000037500704,0.000016641925,0.9939553,0.000011982396,0.0000111544405,0.000045974197,0.0018411633,0.0029836134,0.0005333266,0.000056568002,0.00052768376,0.000012887642],"about_ca_topic_score_codex":0.9802049,"about_ca_topic_score_gemma":0.99341995,"teacher_disagreement_score":0.01979512,"about_ca_system_score_codex":0.0120928865,"about_ca_system_score_gemma":0.006953759,"threshold_uncertainty_score":0.08774048},"labels":[],"label_agreement":null},{"id":"W4413239244","doi":"10.1029/2025jb031651","title":"The Significance of Weak Interfaces for the Kinematics and Rheology of the Ductile Deformation of Earth Materials","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Composite Material Mechanics","field":"Engineering","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"RES’EAU-WaterNET","keywords":"Rheology; Creep; Homogenization (climate); Materials science; Anisotropy; Dislocation creep; Geology; Mechanics; Composite material; Physics","score_opus":0.019943272187586576,"score_gpt":0.3102273802941217,"score_spread":0.29028410810653515,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413239244","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93278193,0.0005948182,0.06231252,0.00014045429,0.00003413873,0.000025379648,0.00007762514,0.00014297859,0.003890247],"genre_scores_gemma":[0.99873847,0.000081228754,0.001008586,0.000004010172,0.000003921354,0.0000035229184,0.00002006423,0.000006998895,0.00013327545],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999083,0.00001164595,0.000008937907,0.00002672627,0.00002550613,0.0000188528],"domain_scores_gemma":[0.9996363,0.000117975345,0.00009872403,0.000044484317,0.00006592261,0.000036641668],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029003998,0.00025445488,0.00015590266,0.0009099243,0.00035275743,0.0011375243,0.00030934595,0.0003283516,0.0009768431],"category_scores_gemma":[0.0013415401,0.00019367058,0.00015812079,0.0002648,0.0008070601,0.0011037093,0.00050457206,0.00039029733,0.00020952159],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030921164,0.00019319517,0.10977496,0.00034455367,0.000052206466,0.0009669437,0.00049199763,0.11987625,0.64331526,0.07118534,0.0007158575,0.052774284],"study_design_scores_gemma":[0.000022527722,0.00023459295,0.08501185,0.000032021522,0.000037297294,0.00036018103,0.0003624326,0.76537055,0.110664524,0.036089018,0.0017556107,0.000059481667],"about_ca_topic_score_codex":0.000899356,"about_ca_topic_score_gemma":0.0004940962,"teacher_disagreement_score":0.0011375243,"about_ca_system_score_codex":0.00024322474,"about_ca_system_score_gemma":0.00016906719,"threshold_uncertainty_score":0.0032678246},"labels":[],"label_agreement":null},{"id":"W4414602670","doi":"10.1029/2025jb031674","title":"The Role of Dislocations in the Anelasticity of the Upper Mantle","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Lakehead University","funders":"Division of Earth Sciences; Royal Commission for the Exhibition of 1851; University of Minnesota; National Science Foundation","keywords":"Viscoelasticity; Attenuation; Anisotropy; Grain Boundary Sliding; Grain boundary; Dislocation; Crystallite; Dissipation; Extrapolation","score_opus":0.016320015740513477,"score_gpt":0.3046752142949873,"score_spread":0.2883551985544738,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414602670","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9969312,0.0000921534,0.0026247553,0.00004338827,0.0000015161739,0.0000027349258,0.000029888768,0.000019559646,0.00025480625],"genre_scores_gemma":[0.9995987,0.000025610263,0.00028185037,0.000003297173,6.5838265e-7,0.0000014996235,0.0000131185325,0.0000018879042,0.000073438096],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99994946,0.000008507361,0.000003981567,0.000010823382,0.00001660835,0.000010732193],"domain_scores_gemma":[0.9998646,0.000050369876,0.000026450043,0.00002621854,0.00002177955,0.000010511923],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012270172,0.00014246459,0.00011981112,0.00023265954,0.00015987716,0.000364846,0.00023761239,0.0002008691,0.0006023128],"category_scores_gemma":[0.00040205073,0.00011404711,0.00015106873,0.00012788436,0.0003314192,0.00034245223,0.0002805689,0.00024956185,0.00007789718],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008540637,0.000077773475,0.012801517,0.0000402677,0.00002208317,0.00008147606,0.00007672311,0.030419443,0.9490536,0.0014499815,0.00004683696,0.0058449027],"study_design_scores_gemma":[0.000034565837,0.00022654039,0.07374761,0.000008959094,0.000022739156,0.00012395266,0.00012644913,0.5743401,0.34722888,0.003494727,0.0006098656,0.0000357031],"about_ca_topic_score_codex":0.0026538873,"about_ca_topic_score_gemma":0.0015494019,"teacher_disagreement_score":0.0026538873,"about_ca_system_score_codex":0.00025171158,"about_ca_system_score_gemma":0.00013411121,"threshold_uncertainty_score":0.0052769184},"labels":[],"label_agreement":null},{"id":"W4414815568","doi":"10.1029/2024jb030585","title":"Modeling Overpressure Development and the Mechanical Behavior of Sediments in a Complex, Tectonically Active Setting: East Coast Basin, New Zealand","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Hydraulic Fracturing and Reservoir Analysis","field":"Engineering","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"Durham University","keywords":"Overpressure; Tectonics; Subduction; Structural basin; Pore water pressure; Cretaceous; Compaction","score_opus":0.024023459188467888,"score_gpt":0.3110376923508679,"score_spread":0.28701423316240005,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414815568","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997186,0.000027743028,0.0014060027,0.000054929365,0.0000028400868,0.000020017247,0.00028148614,0.000027685435,0.000993228],"genre_scores_gemma":[0.99816006,0.00004721043,0.0011833489,0.000007928507,0.0000017942066,0.000020221762,0.00013931688,0.0000071467607,0.0004330447],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999095,0.000011454284,0.000008014596,0.000034293334,0.000014803959,0.000021943297],"domain_scores_gemma":[0.99974364,0.0000823031,0.00006609792,0.000021525811,0.00005432308,0.00003198256],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002325329,0.0005585417,0.00030854717,0.00055203965,0.0005737618,0.0013908097,0.0012789054,0.0011485388,0.0013852874],"category_scores_gemma":[0.0010475747,0.00064750994,0.0006890693,0.00066149945,0.00092804397,0.00068669446,0.0006563125,0.0005293788,0.00012861137],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004343913,0.000065363456,0.03835318,0.000025239278,0.0000460763,0.00021494344,0.0000906903,0.9561484,0.0023181252,0.00034718562,0.00009469222,0.0022527114],"study_design_scores_gemma":[0.000026584155,0.000035531688,0.023025312,0.0000056245626,0.000019396573,0.00002272361,0.00007391336,0.97614986,0.0002976116,0.00013897415,0.00019287752,0.000011633943],"about_ca_topic_score_codex":0.46920225,"about_ca_topic_score_gemma":0.30202302,"teacher_disagreement_score":0.46920225,"about_ca_system_score_codex":0.003374471,"about_ca_system_score_gemma":0.0018472149,"threshold_uncertainty_score":0.9329424},"labels":[],"label_agreement":null},{"id":"W4415009194","doi":"10.1029/2025jb031122","title":"Probing the Nature of Low‐Frequency Earthquakes Through the Deconvolution of Tectonic Tremor","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Seismogram; Deconvolution; Residual; Consistency (knowledge bases); Waveform; Moment (physics); Arrival time","score_opus":0.028340976247773427,"score_gpt":0.32346281611221644,"score_spread":0.295121839864443,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415009194","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9854584,0.000044864246,0.013436221,0.00004366185,0.0000027652727,0.000004124966,0.00010985249,0.00009687248,0.00080331025],"genre_scores_gemma":[0.99737984,0.000015201037,0.002265555,0.000004811759,0.0000018190336,0.0000010215527,0.00011287014,0.000009895014,0.00020899824],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992335,0.0000089187715,0.0000032429132,0.0000171691,0.000026897324,0.000020403284],"domain_scores_gemma":[0.9996032,0.00013429133,0.00008073822,0.000045552322,0.00008444033,0.000051632407],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028866835,0.00023308228,0.00015721544,0.00069115934,0.00023004696,0.0004986559,0.00025853954,0.00029575685,0.0007344147],"category_scores_gemma":[0.0013271809,0.00017497459,0.00013979315,0.00045638834,0.00022280561,0.00027031804,0.0002579823,0.0002529969,0.00022897165],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046113934,0.00016561602,0.47545686,0.00009887412,0.00017372008,0.0004903499,0.0006892492,0.08018991,0.3267111,0.0027167127,0.00092712627,0.11191934],"study_design_scores_gemma":[0.000015705245,0.000063400155,0.54178584,0.000011877053,0.000028390885,0.00018319147,0.00020628558,0.42984018,0.025294665,0.0014974228,0.0010408517,0.000032124088],"about_ca_topic_score_codex":0.01447135,"about_ca_topic_score_gemma":0.025598947,"teacher_disagreement_score":0.01447135,"about_ca_system_score_codex":0.00038835252,"about_ca_system_score_gemma":0.000378079,"threshold_uncertainty_score":0.028774261},"labels":[],"label_agreement":null},{"id":"W4415139719","doi":"10.1029/2024jb031083","title":"Contrasting Crustal Signatures Across the 2021 M <sub>S</sub> 6.0 Luxian (China) Induced Earthquake Revealed by Dense Seismic and Magnetotelluric Data","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"National Natural Science Foundation of China","keywords":"Magnetotellurics; Seismic velocity; Fault (geology); Structural basin; Seismotectonics; Anomaly (physics)","score_opus":0.03240947778401692,"score_gpt":0.31985399250716134,"score_spread":0.2874445147231444,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415139719","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99900717,0.000028756887,0.0002230397,0.000024876546,0.0000017082479,0.0000028233012,0.0003178182,0.000018613237,0.00037521616],"genre_scores_gemma":[0.9988133,0.000018893692,0.0002419726,0.000010620183,0.000008176035,0.000004736428,0.00072248076,0.0000036427311,0.00017622104],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998965,0.000009837951,0.00000805048,0.000025424912,0.000027625416,0.000032417734],"domain_scores_gemma":[0.99976045,0.000019520825,0.0000890366,0.000023160184,0.00005286848,0.00005488897],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017735339,0.00026197292,0.00021048912,0.0014309877,0.00020569905,0.0003537946,0.00020678474,0.00020854021,0.0006751514],"category_scores_gemma":[0.00030801576,0.00014915019,0.00016475286,0.0013303788,0.00025405368,0.0002387738,0.00054082857,0.00011461183,0.000116161675],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012889983,0.000058529982,0.8799567,0.00007321539,0.00008256192,0.00062341994,0.00081180746,0.0019248258,0.081819504,0.00031141003,0.00084370916,0.03336537],"study_design_scores_gemma":[0.0000034342718,0.000013446166,0.9980806,0.000001923529,0.000008261852,0.000044051296,0.00009136393,0.0010188607,0.0004451039,0.000020530855,0.00026769075,0.000004751455],"about_ca_topic_score_codex":0.008218076,"about_ca_topic_score_gemma":0.019907964,"teacher_disagreement_score":0.008218076,"about_ca_system_score_codex":0.00021812868,"about_ca_system_score_gemma":0.00021860507,"threshold_uncertainty_score":0.016340494},"labels":[],"label_agreement":null},{"id":"W4415478739","doi":"10.1029/2024jb030041","title":"A Recipe for Exotic Continental Fragment Formation: Key Constraints From Numerical Rift Models","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"Government of Ontario; National Science Foundation","keywords":"Continental margin; Rift; Lithosphere; Continental crust; Subduction; Plate tectonics; Tectonics; Continental drift; Breakup","score_opus":0.05519301490451972,"score_gpt":0.30595341050270175,"score_spread":0.25076039559818203,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415478739","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0541135,0.00019425694,0.9333645,0.0005554364,0.00006973776,0.0001630823,0.00086652377,0.0020201155,0.008652888],"genre_scores_gemma":[0.46603027,0.00022201787,0.5282337,0.00014843838,0.00007317422,0.00052886724,0.0006917271,0.0019234661,0.002148377],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99961346,0.00016402108,0.000028246468,0.00006294665,0.00009442601,0.000036974303],"domain_scores_gemma":[0.9959746,0.0024005272,0.00037501784,0.00051717454,0.00051777804,0.00021483605],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014922183,0.0010080712,0.0011350061,0.0011818627,0.0009769314,0.0016733388,0.0023936534,0.0014328102,0.007794766],"category_scores_gemma":[0.010750203,0.0012240474,0.001155734,0.0005876088,0.00094685826,0.00089565833,0.0016826574,0.001725874,0.0008570502],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012288514,0.000020262654,0.0011757405,0.00005181899,0.00002154923,0.000091553535,0.000055560056,0.9721133,0.0013503851,0.020035958,0.00062146416,0.004450056],"study_design_scores_gemma":[0.000004828692,0.0000037602767,0.00006958447,0.0000067299375,0.0000024310887,0.000008990616,0.000005586289,0.9946077,0.00018160637,0.0045488775,0.0005544566,0.0000055322325],"about_ca_topic_score_codex":0.00923115,"about_ca_topic_score_gemma":0.012010745,"teacher_disagreement_score":0.00923115,"about_ca_system_score_codex":0.0009392214,"about_ca_system_score_gemma":0.0013335783,"threshold_uncertainty_score":0.026076078},"labels":[],"label_agreement":null},{"id":"W4415848504","doi":"10.1029/2025jb031762","title":"Local Rotations Biasing Supercontinental Configurations: Revisiting a Key ca. 780 Ma Paleomagnetic Pole for Laurentia and Rodinia","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"National Key Research and Development Program of China","keywords":"Rodinia; Paleomagnetism; Laurentia; Supercontinent; Apparent polar wander; Clockwise; Mafic; Geomagnetic pole","score_opus":0.025839058036342354,"score_gpt":0.3082841660745232,"score_spread":0.28244510803818085,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415848504","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99509084,0.00032853044,0.00035186458,0.000047680172,0.000009562153,0.000012060588,0.00016369433,0.00001934779,0.003976451],"genre_scores_gemma":[0.99908924,0.000085924716,0.00033186103,0.000014645748,0.000006154243,0.0000037840489,0.00011417204,0.000013304237,0.00034089666],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987125,0.000011292617,0.000006891403,0.000053468175,0.000022548445,0.00003449443],"domain_scores_gemma":[0.99981695,0.000018292045,0.000052922012,0.00002156119,0.000060580853,0.00002978928],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002799218,0.00030552482,0.00028087216,0.0013830398,0.0010808309,0.0012797907,0.00047466758,0.0003064078,0.002535403],"category_scores_gemma":[0.0007053007,0.00015120736,0.00016812306,0.0010841814,0.00071653177,0.0004622124,0.0009652366,0.00031641035,0.00048882206],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043701744,0.000050916846,0.80184704,0.00016928281,0.0000996682,0.001735713,0.0074775885,0.0018059019,0.12445134,0.0013268671,0.00057647115,0.060022194],"study_design_scores_gemma":[0.000009879078,0.000029206662,0.9907607,0.000031571893,0.000022228076,0.00017105458,0.001296245,0.0010926673,0.0019892205,0.00016624125,0.0044219047,0.000009081811],"about_ca_topic_score_codex":0.06556543,"about_ca_topic_score_gemma":0.16395941,"teacher_disagreement_score":0.06556543,"about_ca_system_score_codex":0.0010385984,"about_ca_system_score_gemma":0.00060567237,"threshold_uncertainty_score":0.13036764},"labels":[],"label_agreement":null},{"id":"W4416590703","doi":"10.1029/2025jb032184","title":"Controls on Asymmetric Continental Crustal Thinning to Symmetric Mantle Exhumation at Magma‐Poor Rifted Margins: Processes Constrained by the West Iberia‐Newfoundland Conjugate Margins","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Program for Jilin University Science and Technology Innovative Research Team; National Key Research and Development Program of China; National Science Foundation","keywords":"Lithosphere; Mantle (geology); Shear zone; Thinning; Rift; Rheology; Seafloor spreading; Continental margin","score_opus":0.019471570974476556,"score_gpt":0.2873526778032068,"score_spread":0.26788110682873023,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416590703","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990435,0.000024837129,0.00011487442,0.000018571076,8.828987e-7,0.0000016079708,0.00008418004,0.00000836204,0.0007032762],"genre_scores_gemma":[0.9997733,0.000014748482,0.000034875262,0.0000034250118,2.9241008e-7,0.0000014014083,0.000041423933,0.0000022124252,0.00012840511],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999188,0.0000114799695,0.000004350989,0.000028262806,0.000005213291,0.000031731088],"domain_scores_gemma":[0.999864,0.000026566113,0.00004282717,0.000017769533,0.000016900336,0.000032003434],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017094579,0.00032721378,0.00021914327,0.00025989563,0.00032368297,0.0008888634,0.00033722437,0.00026723047,0.0014335465],"category_scores_gemma":[0.0004897614,0.00026335154,0.0003362869,0.00017516839,0.00045085142,0.00025712186,0.00041880406,0.0001842246,0.00009614751],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006854592,0.00012053674,0.61819553,0.00007732197,0.0003613515,0.000675949,0.00062970415,0.272922,0.09358819,0.002355726,0.0006310598,0.00975716],"study_design_scores_gemma":[0.000027110214,0.00003531097,0.9235033,0.000008615875,0.00005439266,0.000028841669,0.00026878616,0.07277868,0.0026703214,0.00020906112,0.00039769008,0.000017887905],"about_ca_topic_score_codex":0.3340139,"about_ca_topic_score_gemma":0.30664003,"teacher_disagreement_score":0.66598606,"about_ca_system_score_codex":0.0027914562,"about_ca_system_score_gemma":0.0009049239,"threshold_uncertainty_score":0.66413945},"labels":[],"label_agreement":null},{"id":"W4417155620","doi":"10.1029/2025jb032128","title":"Solid‐State Sintering Can Cause Explosivity and Seismogenic Unstable Sliding During Dome‐Building Eruptions","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"National Science Foundation","keywords":"Fault gouge; Sintering; Shear (geology); Lithification; Shear stress; Volcano; Rheology","score_opus":0.0412117374114627,"score_gpt":0.36544426490627696,"score_spread":0.32423252749481424,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4417155620","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9998148,0.00003137882,0.000067577006,0.0000017488552,5.67605e-7,0.0000017705994,0.000012884671,0.0000032676064,0.00006601731],"genre_scores_gemma":[0.9998142,0.000013564708,0.00006523503,0.0000019714814,3.4508156e-7,0.0000015609555,0.000047315687,0.000001595787,0.000054241238],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99989367,0.000013692643,0.000009586914,0.000022719109,0.000032565695,0.000027818438],"domain_scores_gemma":[0.99983525,0.000031322357,0.00005756444,0.000018941235,0.000027777129,0.000029063965],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019176159,0.00021056579,0.00025910835,0.0003116689,0.00024675814,0.00028027856,0.00016128644,0.00027584264,0.000662831],"category_scores_gemma":[0.00029354572,0.00018692829,0.00016197552,0.00021862361,0.0004208014,0.0001520297,0.0002078829,0.00016368572,0.000083586536],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033899263,0.0000358901,0.046482597,0.000037672133,0.0000286773,0.00035354897,0.00015403576,0.00076370075,0.9496751,0.00004215278,0.000026534084,0.0020612322],"study_design_scores_gemma":[0.00001596951,0.0006193108,0.5617228,0.000007723123,0.000030907468,0.00034619358,0.0003798275,0.006396854,0.42999482,0.00006580206,0.00040568094,0.000014137736],"about_ca_topic_score_codex":0.0017998411,"about_ca_topic_score_gemma":0.0039343196,"teacher_disagreement_score":0.0017998411,"about_ca_system_score_codex":0.0002417345,"about_ca_system_score_gemma":0.00010057178,"threshold_uncertainty_score":0.0035786629},"labels":[],"label_agreement":null},{"id":"W7083709226","doi":"10.1029/2024jb031012","title":"Slow Slip in the Cascadia Subduction Zone: Thinking Outside the Plane","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"Plant Pathogens and Fungal Diseases","field":"Biochemistry, Genetics and Molecular Biology","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Episodic tremor and slip; Subduction; Slip (aerodynamics); Shear (geology); Creep; Instability; Viscoelasticity; Oceanic crust; Crust","score_opus":0.021301260187009684,"score_gpt":0.32750560152047414,"score_spread":0.30620434133346447,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7083709226","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95718724,0.0037926284,0.0094259,0.0072999983,0.00011419433,0.00001501137,0.00014417809,0.00009282853,0.021928057],"genre_scores_gemma":[0.9975303,0.0010191179,0.00042964017,0.00008099188,0.000028987397,0.0000028440925,0.00002955743,0.000006550874,0.0008720071],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998975,0.00001878443,0.000006516873,0.000027966149,0.00001782233,0.000031365078],"domain_scores_gemma":[0.99966085,0.000058086018,0.00008763311,0.000042703876,0.00006685398,0.00008392728],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034063729,0.0005362056,0.0003321122,0.00071403175,0.00062214927,0.0022858188,0.00077128777,0.0009483353,0.0019111016],"category_scores_gemma":[0.0009928094,0.00028126448,0.00039235307,0.00059254956,0.0018821008,0.0023339586,0.0010233657,0.0006622331,0.00027652254],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005137824,0.00007574446,0.44123676,0.00051603484,0.00046419818,0.0027823858,0.005516811,0.31091586,0.018621292,0.17936505,0.004414684,0.03557745],"study_design_scores_gemma":[0.000060725517,0.00024884072,0.45191467,0.0002277093,0.00024347585,0.00039351807,0.008621685,0.27841678,0.0019105428,0.23987527,0.017972857,0.000113850365],"about_ca_topic_score_codex":0.055467162,"about_ca_topic_score_gemma":0.032073285,"teacher_disagreement_score":0.055467162,"about_ca_system_score_codex":0.0021112142,"about_ca_system_score_gemma":0.0006274855,"threshold_uncertainty_score":0.11028862},"labels":[],"label_agreement":null}]}