{"meta":{"query_hash":"e3b20213db28","filters":{"venue":"Geological Society of America eBooks"},"cohort_total":188,"direct_labels_cover":0,"predictions_cover":188,"exported":188,"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/e3b20213db28","api":"https://metacan.xera.ac/api/v1/cohort?venue=Geological+Society+of+America+eBooks"},"results":[{"id":"W1837267421","doi":"10.1130/2010.2465(26)","title":"The Carswell impact event, Saskatchewan, Canada: Evidence for a pre-Athabasca multiring basin?","year":2010,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geology and Paleoclimatology Research","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":"Geology; Breccia; Geochemistry; Structural basin; Basement; Reef; Geomorphology; Petrology; Oceanography","score_opus":0.03600273037208119,"score_gpt":0.2848124675824222,"score_spread":0.248809737210341,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1837267421","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.33431512,0.027528247,0.002607843,0.009688771,0.003118133,0.00977884,0.0029007671,0.000401641,0.6096606],"genre_scores_gemma":[0.7549573,0.0006433812,0.0038207618,0.0012598538,0.0002694468,0.000028707094,0.00016174572,0.000020554653,0.23883826],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.997318,0.000110354544,0.0005476205,0.00062177255,0.00048037735,0.0009218464],"domain_scores_gemma":[0.9936748,0.004828194,0.0004900765,0.00053184235,0.00021055143,0.0002645004],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007644076,0.00045151543,0.0007901012,0.00002381873,0.0007885059,0.000027272541,0.0009105713,0.00082797906,0.0013723022],"category_scores_gemma":[0.00021857006,0.0002768435,0.00086123345,0.000029916147,0.0025583352,0.00003733326,0.0001090737,0.0014504703,0.000030017636],"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":[0.0007291314,0.000018066568,0.93086404,0.00023485046,0.0008017299,0.000031162333,0.00089155557,0.00020507524,0.000028571136,0.00016184732,0.0112547865,0.054779187],"study_design_scores_gemma":[0.0012858387,0.0028091052,0.48298913,0.00041411418,0.0004468205,0.00021517108,0.0016201675,0.0046187984,0.00021660027,0.013995992,0.48955187,0.0018363685],"about_ca_topic_score_codex":0.26527032,"about_ca_topic_score_gemma":0.6532597,"teacher_disagreement_score":0.47829708,"about_ca_system_score_codex":0.000014660262,"about_ca_system_score_gemma":0.0012886287,"threshold_uncertainty_score":0.99996835},"labels":[],"label_agreement":null},{"id":"W1909557249","doi":"10.1130/2010.1206(20)","title":"A model for Iapetan rifting of Laurentia based on Neoproterozoic dikes and related rocks","year":2010,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","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; Massif; Rift; Laurentia; Dike; Rodinia; Paleontology; Volcanic rock; Petrology; Geochemistry; Volcano; Geomorphology; Tectonics","score_opus":0.01574227916242384,"score_gpt":0.19127261487154926,"score_spread":0.1755303357091254,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1909557249","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.101514705,0.0013423646,0.014221513,0.0018762122,0.00018408113,0.0020327922,0.0012716432,0.00026257616,0.8772941],"genre_scores_gemma":[0.94619024,0.00004824963,0.02302903,0.0010367767,0.000047927417,0.000006796448,0.00031619877,0.000009865152,0.02931493],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99809057,0.00002277973,0.00063204905,0.00057182554,0.0003237892,0.00035897005],"domain_scores_gemma":[0.99844587,0.00039870042,0.00062057795,0.0002525184,0.00011771357,0.00016464666],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00020896543,0.00037489223,0.0009016083,0.000041849242,0.00015046237,0.000012138822,0.00028653332,0.00069703005,0.0032701138],"category_scores_gemma":[0.000074053474,0.0002510019,0.0008277461,0.000035301888,0.0012134889,0.000016767919,0.000052245832,0.0006625022,0.000009805053],"study_design_candidate":"design_other","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":[0.002375522,0.000549633,0.059292298,0.00222973,0.002892843,0.000030609197,0.0019330623,0.07116605,0.009485733,0.006511422,0.0020844177,0.84144866],"study_design_scores_gemma":[0.00078388373,0.0016973509,0.0019038832,0.00014725345,0.0004710711,0.0000040833197,0.000058625334,0.7444656,0.0003585791,0.24329974,0.0060790842,0.0007308835],"about_ca_topic_score_codex":0.00028274852,"about_ca_topic_score_gemma":0.00006142634,"teacher_disagreement_score":0.8479792,"about_ca_system_score_codex":0.0000024531128,"about_ca_system_score_gemma":0.000030016045,"threshold_uncertainty_score":0.9999942},"labels":[],"label_agreement":null},{"id":"W1917304467","doi":"10.1130/0-8137-2393-0.329","title":"Middle Jurassic Topawa Group, Baboquivari Mountains, south-central Arizona: Volcanic and sedimentary record of deep basins within the Jurassic magmatic arc","year":2005,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","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; Breccia; Conglomerate; Rhyolite; Pyroclastic rock; Geochemistry; Sedimentary rock; Clastic rock; Siltstone; Volcanic rock; Lithology; Basalt; Diorite; Dacite; Lava; Petrology; Geomorphology; Volcano; Structural basin; Zircon; Facies","score_opus":0.013489598189334338,"score_gpt":0.1779283524335942,"score_spread":0.16443875424425985,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1917304467","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.49858925,0.009468138,0.0020149983,0.007000052,0.0006387984,0.0022630019,0.0015025348,0.00032127777,0.47820196],"genre_scores_gemma":[0.9654959,0.0006257927,0.010702796,0.0048411554,0.00036963,0.00000892661,0.00042685514,0.000019575138,0.017509412],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9966665,0.00011566118,0.0010536835,0.0007910519,0.00066550745,0.00070757687],"domain_scores_gemma":[0.9976203,0.00052593584,0.000984093,0.00045616785,0.00009255977,0.00032095754],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003386399,0.0006301757,0.0012554529,0.000046991994,0.0002652131,0.000034891484,0.0006685855,0.0005070319,0.008599958],"category_scores_gemma":[0.000044167828,0.0003723911,0.00090605696,0.000097350945,0.002944167,0.000058473524,0.00019608247,0.0009317874,0.00005659153],"study_design_candidate":"design_other","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":[0.00084723206,0.0004758271,0.20713326,0.0011008901,0.00414383,0.00007330198,0.0054391907,0.0014177976,0.0005673662,0.012901459,0.003934525,0.76196533],"study_design_scores_gemma":[0.0032882246,0.0067335297,0.30171335,0.00071766216,0.0043631624,0.00014469656,0.00720747,0.06091806,0.00021100767,0.45259678,0.15723346,0.0048726113],"about_ca_topic_score_codex":0.0019901693,"about_ca_topic_score_gemma":0.0010493253,"teacher_disagreement_score":0.7570927,"about_ca_system_score_codex":0.000023158333,"about_ca_system_score_gemma":0.00005545974,"threshold_uncertainty_score":0.9998728},"labels":[],"label_agreement":null},{"id":"W1919391388","doi":"10.1130/2007.2425(06)","title":"Remotely triggered earthquakes following moderate main shocks","year":2007,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"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; Intraplate earthquake; Geology; Aftershock; Remotely triggered earthquakes; Induced seismicity; Volcano; Earthquake swarm; Tectonics; Geothermal gradient; Seismic gap; Depth of focus (tectonics); Geophysics; Subduction","score_opus":0.04205080467832955,"score_gpt":0.23609686238025174,"score_spread":0.19404605770192218,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1919391388","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.007661962,0.0034702427,0.000913716,0.00015465735,0.0002454629,0.00038041468,0.00012010034,0.0001629683,0.9868905],"genre_scores_gemma":[0.4410526,0.0017802811,0.02064112,0.003945198,0.00050609256,0.0000027549968,0.00023491301,0.000044230972,0.5317928],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9970752,0.00004929922,0.0007233057,0.0007187249,0.0006760854,0.00075739773],"domain_scores_gemma":[0.9982752,0.0006053694,0.00044559507,0.00039139047,0.000073363415,0.00020909018],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00039702648,0.0005840535,0.0012121183,0.00006651429,0.00036198375,0.000036060253,0.00039018932,0.0006950643,0.0038496125],"category_scores_gemma":[0.000039862072,0.00045271774,0.0014320386,0.000051838095,0.0009838252,0.000043492924,0.00007643372,0.00080691034,0.0002658813],"study_design_candidate":"design_other","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":[0.00023485566,0.000022397695,0.0020924392,0.0000871125,0.0011232082,0.00017105177,0.00081608095,0.0001947993,0.000017697288,0.0013115265,0.0052751345,0.9886537],"study_design_scores_gemma":[0.0026328932,0.0031643559,0.040195443,0.0006041048,0.00077386026,0.0000956447,0.001548211,0.004488604,0.00018360665,0.09065372,0.852005,0.003654534],"about_ca_topic_score_codex":0.00057909085,"about_ca_topic_score_gemma":0.00014658844,"teacher_disagreement_score":0.9849992,"about_ca_system_score_codex":0.000012401452,"about_ca_system_score_gemma":0.000094023235,"threshold_uncertainty_score":0.99979246},"labels":[],"label_agreement":null},{"id":"W1937481124","doi":"10.1130/2006.2397(06)","title":"Building the American Mineralogist Crystal Structure Database: A recipe for construction of a small Internet database","year":2006,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Railway Systems and Materials Science","field":"Engineering","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":"","keywords":"The Internet; Database; Construct (python library); World Wide Web; Software; Computer science; General partnership; Political science","score_opus":0.019657961507306455,"score_gpt":0.2225523232544418,"score_spread":0.20289436174713535,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1937481124","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.13510126,0.0015022462,0.7422303,0.00028692477,0.0022738548,0.004068185,0.014375988,0.00072978303,0.09943143],"genre_scores_gemma":[0.29406714,0.00032081053,0.675243,0.0005692333,0.0011801594,0.00014682472,0.0010750932,0.00020191692,0.027195804],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.9981634,0.000028568062,0.0007157752,0.00045487043,0.000268382,0.00036898835],"domain_scores_gemma":[0.9983452,0.0002144056,0.00073679985,0.0005086626,0.00012172716,0.00007320336],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00022360723,0.00040545498,0.00091596704,0.00004109719,0.00007493141,0.000029997967,0.00052996207,0.0002003828,0.000064874184],"category_scores_gemma":[0.000030498497,0.00029028638,0.00036072748,0.00004462404,0.0025257878,0.000038303857,0.00020535069,0.00031317028,9.443366e-7],"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":[0.00017963948,0.000030790026,0.0000388547,0.0018572176,0.0005573507,0.0000076575325,0.00041068727,0.0029859392,0.8426382,0.03554881,0.06019108,0.05555376],"study_design_scores_gemma":[0.0013599847,0.0017171919,0.00023490124,0.0011957462,0.0005450006,0.00020585557,0.0006750371,0.01981758,0.036890246,0.012849912,0.92214376,0.0023647759],"about_ca_topic_score_codex":0.00079717446,"about_ca_topic_score_gemma":0.00002737005,"teacher_disagreement_score":0.86195266,"about_ca_system_score_codex":0.000055932655,"about_ca_system_score_gemma":0.00003669455,"threshold_uncertainty_score":0.99995494},"labels":[],"label_agreement":null},{"id":"W2104482682","doi":"10.1130/0-8137-2389-2.141","title":"Deciphering the petrogenesis of deeply buried granites: whole-rock geochemical constraints on the origin of largely undepleted felsic granulites from the Moldanubian Zone of the Bohemian Massif","year":2004,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":136,"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":"Austrian Science Fund","keywords":"Felsic; Granulite; Massif; Geology; Geochemistry; Metamorphism; Petrogenesis; Quartz; Petrology; Feldspar; Crust; Continental crust; Metamorphic rock; Mafic; Geomorphology; Basalt","score_opus":0.022523461670343206,"score_gpt":0.19092924319233068,"score_spread":0.16840578152198749,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2104482682","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9093351,0.002008027,0.00035788934,0.008296937,0.00012987481,0.0011618873,0.0024849807,0.000069106325,0.07615625],"genre_scores_gemma":[0.99557364,0.00014244935,0.00071498513,0.0018662061,0.000097989,0.0000068069417,0.0001449734,0.000011263304,0.0014417053],"study_design_codex":"observational","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.996667,0.00019805001,0.0010581576,0.00058988883,0.00096619054,0.0005206646],"domain_scores_gemma":[0.9944948,0.003078216,0.0012094816,0.0008680757,0.0002189906,0.00013045427],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00042972338,0.0005478523,0.0011623399,0.000022546383,0.00032885277,0.000019697647,0.0017380824,0.0004838227,0.006559606],"category_scores_gemma":[0.0002386297,0.00022042583,0.0017460029,0.00021302904,0.0060779303,0.000019643036,0.00023190888,0.0009447341,0.000018447035],"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":[0.0034559479,0.0018403662,0.46471933,0.0014581226,0.019946296,0.00006892127,0.013750806,0.016983654,0.10681648,0.06416861,0.011337368,0.2954541],"study_design_scores_gemma":[0.0039088503,0.0029007401,0.22763114,0.0021366174,0.0046004904,0.000037643225,0.010545131,0.004178468,0.054122943,0.6365083,0.050230265,0.0031994095],"about_ca_topic_score_codex":0.0036296344,"about_ca_topic_score_gemma":0.00016357344,"teacher_disagreement_score":0.5723397,"about_ca_system_score_codex":0.000015816076,"about_ca_system_score_gemma":0.00011121348,"threshold_uncertainty_score":0.996627},"labels":[],"label_agreement":null},{"id":"W2108883396","doi":"10.1130/2014.0037(02)","title":"Sedimentary record of glacial Lake Missoula along the Clark Fork River from deep to shallow positions in the former lakes","year":2014,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":"Government of Saskatchewan","funders":"University of Montana","keywords":"Geology; Precambrian; Paleontology; Glacial period; Tectonics; Sedimentary rock; Archaeology; Geomorphology; Geography","score_opus":0.020327046993862515,"score_gpt":0.2292672541070199,"score_spread":0.2089402071131574,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2108883396","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.32961574,0.0013760641,0.0008558524,0.010399372,0.0003810824,0.0017807954,0.0007814732,0.00005239575,0.6547572],"genre_scores_gemma":[0.9484009,0.00040831062,0.007995235,0.022229526,0.00037096912,0.000028907212,0.0011884376,0.000015840798,0.019361831],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979772,0.0002477021,0.0004947631,0.0004108162,0.00039444419,0.00047509716],"domain_scores_gemma":[0.9974717,0.001707107,0.00026736088,0.00038759504,0.00006784918,0.000098422985],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00045676788,0.0002895585,0.00062457647,0.000042369113,0.00029707619,0.0000114439445,0.0008280368,0.000572956,0.005174169],"category_scores_gemma":[0.000035230107,0.0001636701,0.0004782162,0.00005539112,0.0021733914,0.000022845576,0.00008820604,0.00091098016,0.00015088888],"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":[0.000239191,0.000029331803,0.9643625,0.000032491913,0.0002845648,0.000020311834,0.0043471637,0.00009432293,0.000003296995,0.00074754894,0.00481543,0.025023863],"study_design_scores_gemma":[0.00067652616,0.0015017897,0.69848305,0.00012555334,0.00024212216,0.000036761783,0.0018371203,0.000563658,0.000009007343,0.06672174,0.22921169,0.0005910046],"about_ca_topic_score_codex":0.0025365565,"about_ca_topic_score_gemma":0.023532543,"teacher_disagreement_score":0.6353954,"about_ca_system_score_codex":0.0000028216891,"about_ca_system_score_gemma":0.000050046925,"threshold_uncertainty_score":0.9957352},"labels":[],"label_agreement":null},{"id":"W2115986887","doi":"10.1130/2010.1206(16)","title":"Middle Cambrian to Ordovician arc-backarc development on the leading edge of Ganderia, Newfoundland Appalachians","year":2010,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":71,"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; Rift; Magmatism; Back-arc basin; Ophiolite; Ordovician; Paleontology; Volcanic arc; Earth science; Transtension; Island arc; Basement; Geochemistry; Subduction; Structural basin; Tectonics; Archaeology; Geography","score_opus":0.028550424701159784,"score_gpt":0.19881187367763897,"score_spread":0.17026144897647918,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2115986887","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.13827291,0.00014253262,0.0003494686,0.0019891728,0.00013610123,0.0005127833,0.00010148743,0.000058661863,0.8584369],"genre_scores_gemma":[0.7769892,0.00011345968,0.012539234,0.008323042,0.000322165,0.000010932701,0.0002502104,0.000018860823,0.2014329],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9975254,0.000050252707,0.0006783416,0.00062940293,0.00056191644,0.000554677],"domain_scores_gemma":[0.9982325,0.0005375409,0.0003872124,0.00042182775,0.0001209055,0.0003000174],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00032228878,0.00047291606,0.00097576046,0.000052581003,0.00030265385,0.000025553516,0.0007227732,0.0004984941,0.009836454],"category_scores_gemma":[0.00007420274,0.00026748143,0.0006781462,0.00008475347,0.0013063591,0.00001480446,0.00012822353,0.00089458155,0.0005316329],"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":[0.0011063347,0.0005294941,0.24600191,0.0006571149,0.003678061,0.00006499165,0.008198069,0.001375957,0.007694483,0.025246225,0.007011256,0.6984361],"study_design_scores_gemma":[0.00061559514,0.002091445,0.084258504,0.00034800387,0.00034483036,0.000015417554,0.0007601819,0.00042938648,0.0012279723,0.056357216,0.8516964,0.0018550627],"about_ca_topic_score_codex":0.0020754908,"about_ca_topic_score_gemma":0.004722439,"teacher_disagreement_score":0.84468514,"about_ca_system_score_codex":0.0000127274325,"about_ca_system_score_gemma":0.00008120153,"threshold_uncertainty_score":0.99997777},"labels":[],"label_agreement":null},{"id":"W2205650864","doi":"10.1130/2008.442(10)","title":"Late Triassic silicified shallow-water corals and other marine fossils from Wrangellia and the Alexander terrane, Alaska, and Vancouver Island, British Columbia","year":2008,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Coral and Marine Ecosystems Studies","field":"Environmental Science","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":"","keywords":"Terrane; Geology; Oceanography; Waves and shallow water; Archaeology; Geography; Paleontology","score_opus":0.013901616781368736,"score_gpt":0.18010769068532706,"score_spread":0.16620607390395833,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2205650864","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.39909935,0.0016214587,0.000034459696,0.00031352794,0.00016678436,0.0012962088,0.00019798242,0.00007328196,0.59719694],"genre_scores_gemma":[0.19078161,0.0036182702,0.00040045084,0.0022287045,0.000132059,0.00005958073,0.000018123012,0.000041062773,0.8027201],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99819815,0.000056898978,0.00045076973,0.0006588354,0.00027968988,0.00035565422],"domain_scores_gemma":[0.9991663,0.00022735765,0.0002495628,0.00022568926,0.000015917307,0.000115181465],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00017111008,0.000342069,0.0009783746,0.000006506566,0.00034689507,0.000073330775,0.0001679388,0.00030142118,0.0056788255],"category_scores_gemma":[0.000008096051,0.00024801274,0.00024490026,0.000013418381,0.00358859,0.000037945574,0.0011222379,0.0003279335,0.000015837535],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006667442,0.000107807144,0.158328,0.00017886354,0.0013773331,0.00008194502,0.004995707,0.0000035964674,0.00031295494,0.000027863856,0.51110834,0.32281086],"study_design_scores_gemma":[0.0060250363,0.00050082133,0.14728974,0.00014877562,0.00038487487,0.0000668409,0.0003066757,0.00027693753,0.0000097671955,0.01859427,0.825271,0.0011252719],"about_ca_topic_score_codex":0.04041836,"about_ca_topic_score_gemma":0.043538198,"teacher_disagreement_score":0.3216856,"about_ca_system_score_codex":0.00002644015,"about_ca_system_score_gemma":0.000004808817,"threshold_uncertainty_score":0.9999972},"labels":[],"label_agreement":null},{"id":"W2236151505","doi":"10.1130/2013.4121(13)","title":"The shortcomings of “passive” urban river restoration after low-head dam removal, Ottawa River (northwestern Ohio, USA)","year":2013,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","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":"","keywords":"Subtitle; Dam removal; Head (geology); Hydrology (agriculture); Environmental science; Geology; Geomorphology; Geotechnical engineering","score_opus":0.011212752913923535,"score_gpt":0.20918676214071757,"score_spread":0.19797400922679403,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2236151505","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.44969606,0.0005839514,0.0009277781,0.00062440016,0.00023176747,0.0011516712,0.00007123975,0.000094455696,0.5466187],"genre_scores_gemma":[0.7250794,0.0005059369,0.0034260494,0.0021242239,0.00011025912,0.00007844868,0.000054182456,0.00004580334,0.26857567],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9974282,0.000054372103,0.0007625199,0.00065381406,0.00063598744,0.00046515165],"domain_scores_gemma":[0.9983193,0.00021482933,0.0007401545,0.0005253037,0.000061164385,0.00013924643],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00021962197,0.00046726453,0.0006726487,0.000019459128,0.00026903863,0.000014454271,0.0006172067,0.00070905854,0.0056727184],"category_scores_gemma":[0.0000118473545,0.00031895257,0.0005542828,0.00003783855,0.007432341,0.00012112696,0.0002620737,0.000611175,0.00031680454],"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":[0.0021840378,0.0012714895,0.30916756,0.0010774188,0.0034273616,0.00041759136,0.03605595,0.0013785905,0.0067585316,0.0130344285,0.20735805,0.41786897],"study_design_scores_gemma":[0.0005462135,0.0008417106,0.06347802,0.00013671501,0.00028068613,0.000015879126,0.00008743173,0.00020253718,0.00032279268,0.0077914717,0.9254619,0.00083464786],"about_ca_topic_score_codex":0.0005183561,"about_ca_topic_score_gemma":0.00008659709,"teacher_disagreement_score":0.7181038,"about_ca_system_score_codex":0.00008132648,"about_ca_system_score_gemma":0.000034710425,"threshold_uncertainty_score":0.99992627},"labels":[],"label_agreement":null},{"id":"W2239854719","doi":"10.1130/2007.2425(09)","title":"Effects of a lithospheric weak zone on postglacial seismotectonics in eastern Canada and the northeastern United States","year":2007,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Seismotectonics; Geology; Lithosphere; Seismology; Paleontology; Tectonics","score_opus":0.010972149160966465,"score_gpt":0.18931644254174052,"score_spread":0.17834429338077404,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2239854719","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.67646664,0.007804131,0.00019933148,0.00064447767,0.0003410128,0.0014264279,0.00020813766,0.00005575395,0.31285408],"genre_scores_gemma":[0.9454829,0.00282767,0.00055839174,0.004627876,0.00009561876,0.000004078829,0.00010406332,0.000019256733,0.046280123],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99833256,0.000073361436,0.00045257978,0.0003320472,0.00044190692,0.00036751688],"domain_scores_gemma":[0.9978184,0.0014636134,0.0003822654,0.00018323207,0.00006723643,0.00008525256],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023862816,0.00033633987,0.0007947597,0.000034121957,0.00009973645,0.000008916253,0.00022177615,0.00022722519,0.00016508103],"category_scores_gemma":[0.000031534346,0.00020457321,0.00021258318,0.000070813294,0.0015166446,0.000010686017,0.00006610361,0.0005434742,0.0000055242326],"study_design_candidate":"design_other","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":[0.002643338,0.00008736498,0.08607089,0.00093231903,0.0013633462,0.00015950057,0.005827175,0.0023292145,0.0000027066708,0.00222326,0.0004806642,0.8978802],"study_design_scores_gemma":[0.011763119,0.0073554157,0.48186004,0.0016988452,0.0007029055,0.000058275837,0.0045559662,0.048577342,0.00008553813,0.010528766,0.43002233,0.0027914739],"about_ca_topic_score_codex":0.5973878,"about_ca_topic_score_gemma":0.2206575,"teacher_disagreement_score":0.89508873,"about_ca_system_score_codex":0.000011793427,"about_ca_system_score_gemma":0.000111930574,"threshold_uncertainty_score":0.83422536},"labels":[],"label_agreement":null},{"id":"W2253570008","doi":"10.1130/0-8137-2375-2.25","title":"The Las Colinas landslide, Santa Tecla: A highly destructive flowslide triggered by the January 13, 2001, El Salvador earthquake","year":2004,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":43,"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; Canadian Natural Resources Limited","keywords":"Landslide; Escarpment; Geology; Debris; Geomorphology; Landslide classification; Landslide mitigation; Channelized; Geotechnical engineering","score_opus":0.00885786631526377,"score_gpt":0.20772636478227302,"score_spread":0.19886849846700924,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2253570008","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.017092707,0.0022736338,0.00027561773,0.0029763046,0.00034845056,0.0017163113,0.00026274004,0.00019885512,0.97485536],"genre_scores_gemma":[0.25236344,0.011492451,0.0042082984,0.0071922997,0.00062061806,0.00020625464,0.0002000746,0.00020286797,0.7235137],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9965414,0.000106385254,0.00078203535,0.00080888113,0.0008756302,0.00088566396],"domain_scores_gemma":[0.99767995,0.0005728628,0.00071828376,0.0007396882,0.00004602568,0.00024316297],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00047636975,0.00068040803,0.00089015195,0.000015225997,0.00095082255,0.000063251275,0.0010760198,0.0009519903,0.0012947656],"category_scores_gemma":[0.000042121872,0.00033510212,0.0010395414,0.00008240723,0.0061203274,0.000047412792,0.0007313722,0.0014767972,0.00031425868],"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":[0.0010008707,0.00027063422,0.0013065354,0.00008065981,0.0023558275,0.00010683561,0.00302522,0.0010629524,0.00096636417,0.009385655,0.7653401,0.21509838],"study_design_scores_gemma":[0.0013927065,0.00079443015,0.002128651,0.000099756435,0.00036615145,0.00007158882,0.0007292563,0.00014186966,0.00016433539,0.047238458,0.9460074,0.00086543005],"about_ca_topic_score_codex":0.0014511967,"about_ca_topic_score_gemma":0.00008774572,"teacher_disagreement_score":0.25134167,"about_ca_system_score_codex":0.00025485846,"about_ca_system_score_gemma":0.00010351075,"threshold_uncertainty_score":0.9999101},"labels":[],"label_agreement":null},{"id":"W2266847816","doi":"10.1130/0-8137-2349-3.105","title":"Syntexis and the genesis of lower oceanic crust","year":2000,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","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":"Geology; Geochemistry; Massif; Protolith; Ophiolite; Plagioclase; Anorthosite; Olivine; Crust; Pyroxene; Basalt; Fractional crystallization (geology); Metamorphism; Paleontology; Quartz","score_opus":0.011087791250714872,"score_gpt":0.1744131442621267,"score_spread":0.16332535301141182,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2266847816","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.03183859,0.004461812,0.000039246734,0.0006944303,0.00004063243,0.00026392593,0.00015334165,0.000039197268,0.9624688],"genre_scores_gemma":[0.9172801,0.0052726804,0.0017004424,0.002958567,0.00012331623,0.0000024204805,0.000081396414,0.000008404535,0.072572716],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99820244,0.000056963312,0.0005657678,0.00046420193,0.00038671665,0.0003238916],"domain_scores_gemma":[0.99839884,0.0006786708,0.0004094469,0.00030688077,0.00007020336,0.00013595638],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00021631118,0.00034878397,0.0010469907,0.000022675385,0.00012891894,0.0000121779985,0.00042591913,0.00039717718,0.031519506],"category_scores_gemma":[0.000031884923,0.00017982187,0.0010047142,0.000046529032,0.0046453704,0.000016292995,0.000091522656,0.000409436,0.000072626994],"study_design_candidate":"design_other","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":[0.0021507572,0.00013235287,0.01694841,0.00033626327,0.0027913442,0.000043163753,0.00095229695,0.00046618204,0.00010049039,0.020058613,0.008422307,0.9475978],"study_design_scores_gemma":[0.002049911,0.0021501398,0.040093232,0.00019821023,0.0017509267,0.00006163244,0.000719517,0.005425032,0.00009488785,0.7070376,0.23873259,0.0016862849],"about_ca_topic_score_codex":0.0022466814,"about_ca_topic_score_gemma":0.000016657086,"teacher_disagreement_score":0.9459115,"about_ca_system_score_codex":0.0000024428346,"about_ca_system_score_gemma":0.000022174496,"threshold_uncertainty_score":0.99806345},"labels":[],"label_agreement":null},{"id":"W2276093622","doi":"10.1130/9780813700243","title":"Archean to Anthropocene: Field Guides to the Geology of the Mid-Continent of North America","year":2011,"lang":"en","type":"book","venue":"Geological Society of America eBooks","topic":"Archaeology and Natural History","field":"Social Sciences","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":"Precambrian; Geology; Archaeology; Phanerozoic; Historical geology; Glacial period; Limnology; Earth science; Structural geology; Paleontology; Oceanography; Geography; Cenozoic; Structural basin","score_opus":0.024815108941752442,"score_gpt":0.27148067516659635,"score_spread":0.24666556622484392,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2276093622","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.021702744,0.0032665003,0.002146776,0.042866077,0.0014671804,0.0028447695,0.000131604,0.00012073832,0.9254536],"genre_scores_gemma":[0.30867907,0.0034369535,0.022036888,0.040445484,0.0009590907,0.0001456912,0.00003118549,0.000066278866,0.62419933],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99734527,0.00044538092,0.00067629403,0.0004556315,0.0005117076,0.00056573295],"domain_scores_gemma":[0.99716,0.0009173955,0.0008202121,0.00061905384,0.00031398144,0.00016934058],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0004738437,0.0003025886,0.0009144194,0.00004598025,0.0005117533,0.0000010337783,0.0017647141,0.0005216524,0.0006087092],"category_scores_gemma":[0.00050197646,0.00017722271,0.0008479877,0.00017801071,0.012606232,0.000015512152,0.0010113158,0.00077058875,0.000023127737],"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":[0.00034634318,0.0001686234,0.008759991,0.000116789575,0.00044900915,0.000003640015,0.071693346,0.00003563456,0.00009211044,0.0039960025,0.6626375,0.25170103],"study_design_scores_gemma":[0.00009907323,0.00080865825,0.006743204,0.00005027521,0.00007502283,9.828574e-7,0.0011820741,0.0000017910263,0.0002289641,0.005525185,0.9850492,0.00023560273],"about_ca_topic_score_codex":0.0062332223,"about_ca_topic_score_gemma":0.0011220463,"teacher_disagreement_score":0.3224117,"about_ca_system_score_codex":0.00009360415,"about_ca_system_score_gemma":0.0004951508,"threshold_uncertainty_score":0.9900809},"labels":[],"label_agreement":null},{"id":"W2277116935","doi":"10.1130/2014.2505(11)","title":"The Pliensbachian–Toarcian (Early Jurassic) extinction: A North American perspective","year":2014,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":58,"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":"Durham University; Natural Environment Research Council; Sight Research UK","keywords":"Perspective (graphical); Paleontology; Geology; Extinction (optical mineralogy); Artificial intelligence; Computer science","score_opus":0.00998749167926336,"score_gpt":0.20282811879833862,"score_spread":0.19284062711907526,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2277116935","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.006691597,0.0001816166,0.000717799,0.001113662,0.00014686577,0.00047161191,0.000018357192,0.00010031982,0.99055815],"genre_scores_gemma":[0.12698913,0.0009954699,0.0047241063,0.0032940777,0.00047314257,0.00006677512,0.000024643647,0.000114128685,0.8633185],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99722934,0.00009661237,0.00059118756,0.0008045784,0.00064970105,0.0006285675],"domain_scores_gemma":[0.9977403,0.0003266808,0.0010005141,0.0006291098,0.00005185039,0.0002515244],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00027754367,0.00052922865,0.0007536027,0.000016858692,0.0006142037,0.000038211983,0.00067012385,0.00028572042,0.0015331194],"category_scores_gemma":[0.000026220434,0.00032732077,0.00077723275,0.000085356485,0.0069276616,0.00002220454,0.00054888154,0.0011131625,0.0005693576],"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":[0.00033942642,0.00015004288,0.0056811054,0.000040688607,0.0014465937,0.000022290891,0.0073405956,0.0006371843,0.00017719736,0.034886923,0.03351303,0.9157649],"study_design_scores_gemma":[0.0002896308,0.0012735969,0.011229289,0.00002139839,0.00015682711,0.000010750045,0.0009225039,0.00033014666,0.000009289111,0.0132517135,0.9717725,0.0007323391],"about_ca_topic_score_codex":0.0007550372,"about_ca_topic_score_gemma":0.00006850129,"teacher_disagreement_score":0.9382595,"about_ca_system_score_codex":0.00026605764,"about_ca_system_score_gemma":0.000026699177,"threshold_uncertainty_score":0.99991786},"labels":[],"label_agreement":null},{"id":"W2288926948","doi":"10.1130/2014.2503(09)","title":"Diversity and paleoecology of actinopterygian fish from vertebrate microfossil localities of the Maastrichtian Hell Creek Formation of Montana","year":2014,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Paleontology and Evolutionary Biology","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":false,"ca_institutions":"Royal Tyrrell Museum","funders":"University of California Museum of Paleontology","keywords":"Vertebrate; Catfish; Paleoecology; Fish <Actinopterygii>; Paleontology; Taphonomy; Biology; Assemblage (archaeology); Cretaceous; Geology; Ecology; Fishery","score_opus":0.015887498450123147,"score_gpt":0.17101711228722022,"score_spread":0.15512961383709706,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2288926948","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8766525,0.001249657,0.0006924105,0.00026412308,0.00021892242,0.0003270502,0.0009796318,0.000016980677,0.11959872],"genre_scores_gemma":[0.9941422,0.00032335383,0.00058324594,0.00038288118,0.000025323974,4.1281203e-7,0.00008396447,0.0000018218502,0.004456809],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9988382,0.00012506865,0.00045577693,0.0002303897,0.00014929366,0.00020130453],"domain_scores_gemma":[0.9983538,0.00042694373,0.0008816211,0.00019909911,0.00008578272,0.000052787927],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00014770961,0.00018073985,0.00067793374,0.000023726676,0.0002819752,0.0000013752602,0.0003315689,0.0005247251,0.0005820117],"category_scores_gemma":[0.00002136192,0.00013272297,0.0002879925,0.000019965055,0.003430344,0.000028452738,0.00024318125,0.0002597518,0.0000024519818],"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":[0.0002303983,0.000020068892,0.9611194,0.00018229471,0.00030629148,0.0000017572671,0.0023194216,0.000030133364,0.00009956923,0.00027611747,0.0012280898,0.03418643],"study_design_scores_gemma":[0.00044383644,0.0008783861,0.98065,0.00006399764,0.00018303943,0.000011287756,0.00073832803,0.00064271846,0.0001904445,0.008049246,0.00792896,0.00021977401],"about_ca_topic_score_codex":0.0037576607,"about_ca_topic_score_gemma":0.003976784,"teacher_disagreement_score":0.11748968,"about_ca_system_score_codex":0.000004993505,"about_ca_system_score_gemma":0.000032678003,"threshold_uncertainty_score":0.99928176},"labels":[],"label_agreement":null},{"id":"W2309440933","doi":"10.1130/0-8137-2343-4.257","title":"Metamorphic history of the Coast Mountains orogen, western British Columbia and southeastern Alaska","year":2000,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","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; Metamorphic rock; Archaeology; Seismology; Oceanography; Geography; Paleontology","score_opus":0.013876446861073293,"score_gpt":0.16305204363660203,"score_spread":0.14917559677552875,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2309440933","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.43037486,0.008146379,0.00002814041,0.0004145622,0.00017737673,0.0005648368,0.0009123644,0.00008757405,0.5592939],"genre_scores_gemma":[0.6020847,0.00083221495,0.0004648208,0.0021677467,0.00008858031,0.0000028924244,0.00010301137,0.00001062015,0.39424545],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9978616,0.00007267104,0.00061287923,0.0005753671,0.0004949734,0.0003824778],"domain_scores_gemma":[0.99865586,0.00018486728,0.00053960417,0.00034069634,0.00009160557,0.00018739508],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00015157174,0.00030604532,0.0010094972,0.000013817742,0.000121019846,0.000031633685,0.0005238175,0.0004511088,0.02221439],"category_scores_gemma":[0.000017251696,0.00025236697,0.00092390523,0.00003604108,0.0034460053,0.000024934407,0.00015224937,0.00054622605,0.00004062526],"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":[0.00008149626,0.00009518158,0.77941906,0.00023235557,0.0011438146,0.000031065698,0.0007892275,0.00012918298,0.00006863299,0.00007266969,0.010480966,0.20745635],"study_design_scores_gemma":[0.0008188596,0.0009264392,0.3582827,0.00027845317,0.0012070602,0.0001407549,0.00043988365,0.00079420995,0.000010809336,0.06604679,0.5696959,0.0013581378],"about_ca_topic_score_codex":0.040349837,"about_ca_topic_score_gemma":0.01976992,"teacher_disagreement_score":0.55921495,"about_ca_system_score_codex":0.000011790819,"about_ca_system_score_gemma":0.00007489524,"threshold_uncertainty_score":0.99999285},"labels":[],"label_agreement":null},{"id":"W2310212265","doi":"10.1130/0-8137-1197-5.35","title":"Granulite-facies P-T-t paths and the influence of retrograde cation diffusion during polyphase orogenesis, western Grenville Province, Québec","year":2004,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":11,"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 Sciences and Engineering Research Council of Canada; Université du Québec à Chicoutimi","keywords":"Granulite; Geology; Polyphase system; Geochemistry; Facies; Petrology; Diffusion; Shear zone; Geomorphology; Seismology; Tectonics; Thermodynamics","score_opus":0.0073343343703604425,"score_gpt":0.18977785047429438,"score_spread":0.18244351610393394,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2310212265","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8923899,0.0046432777,0.0061157336,0.008308163,0.00011787077,0.0020832191,0.000059814996,0.00038103896,0.08590101],"genre_scores_gemma":[0.9623881,0.0006905958,0.0032787677,0.00049857155,0.000044523335,0.000030516414,0.000009591806,0.000009257193,0.033050064],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9979404,0.0000532299,0.0006208572,0.00062959956,0.0004196926,0.00033621406],"domain_scores_gemma":[0.99795914,0.00021125517,0.0008874182,0.0006667026,0.00017605751,0.00009940251],"candidate_categories":["metaepi_narrow","sts"],"consensus_categories":[],"category_scores_codex":[0.00023185168,0.00039268247,0.00072142377,0.000030437337,0.00027564933,0.00003259587,0.00083343056,0.00037156575,0.000022930551],"category_scores_gemma":[0.00006828951,0.0002607245,0.0004091281,0.00005266788,0.0028458592,0.00005594516,0.00086710264,0.00039649027,0.000002605379],"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":[0.0017797877,0.0013201041,0.057704046,0.010061385,0.002670977,0.00024993258,0.056343507,0.005767477,0.100567974,0.42312622,0.0007844458,0.33962414],"study_design_scores_gemma":[0.025999023,0.0049157883,0.20028114,0.0055095535,0.001415038,0.00090486574,0.0028667003,0.0047225156,0.033045057,0.36352655,0.3475504,0.009263355],"about_ca_topic_score_codex":0.0021330013,"about_ca_topic_score_gemma":0.00003351267,"teacher_disagreement_score":0.34676597,"about_ca_system_score_codex":0.00005775792,"about_ca_system_score_gemma":0.00018599474,"threshold_uncertainty_score":0.9999845},"labels":[],"label_agreement":null},{"id":"W2312333189","doi":"10.1130/2009.fld015(13)","title":"The Boring Volcanic Field of the Portland-Vancouver area, Oregon and Washington","year":2009,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","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; Volcano; Forearc; Volcanism; Lava; Subtitle; Scoria; Earth science; Seismology; Archaeology; History; Tectonics; Subduction","score_opus":0.009706257070548481,"score_gpt":0.18033181735912168,"score_spread":0.1706255602885732,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2312333189","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.033864085,0.0025458522,0.00003331611,0.0020655633,0.00016457847,0.00035129848,0.00010917383,0.000047836373,0.9608183],"genre_scores_gemma":[0.8578178,0.001430271,0.0005580565,0.003216041,0.00014481384,0.0000020424648,0.000053117696,0.0000059914405,0.13677186],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9984694,0.00003162098,0.00043905864,0.0003527114,0.00038699916,0.0003201984],"domain_scores_gemma":[0.99835837,0.00066842407,0.00048321002,0.00031229254,0.00007678457,0.00010093049],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00017747437,0.00027402578,0.00055035873,0.000011198779,0.00025374445,0.00001702243,0.0004978544,0.0003364028,0.0032702677],"category_scores_gemma":[0.00008763801,0.000121406425,0.00062849873,0.000043159773,0.0009597468,0.000018126895,0.0001241456,0.0005704532,0.0000066229536],"study_design_candidate":"design_other","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":[0.00015034685,0.000032200493,0.042899497,0.000093636416,0.000499333,0.000007888818,0.00027059452,0.00020028501,0.000116058014,0.0016409545,0.03693957,0.91714966],"study_design_scores_gemma":[0.00043818128,0.0014238633,0.06545265,0.00026381857,0.00047922254,0.000013948001,0.00042059415,0.002099638,0.00068779726,0.29185486,0.63595295,0.00091250695],"about_ca_topic_score_codex":0.00092981133,"about_ca_topic_score_gemma":0.00075351633,"teacher_disagreement_score":0.9162371,"about_ca_system_score_codex":0.00000382856,"about_ca_system_score_gemma":0.000026414378,"threshold_uncertainty_score":0.9976409},"labels":[],"label_agreement":null},{"id":"W2320709596","doi":"10.1130/2013.0033(08)","title":"The Laramie anorthosite complex and its contact metamorphic aureole","year":2013,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Amyloidosis: Diagnosis, Treatment, Outcomes","field":"Biochemistry, Genetics and Molecular Biology","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Anorthosite; Geology; Metamorphic rock; Geochemistry; Paleontology; Plagioclase","score_opus":0.02384768474060955,"score_gpt":0.24182900737437676,"score_spread":0.2179813226337672,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2320709596","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.071870364,0.047430806,0.0005186032,0.005046861,0.00033745234,0.0040497337,0.0005711846,0.00021933067,0.86995566],"genre_scores_gemma":[0.58032477,0.014933755,0.0031428577,0.007450152,0.00031706554,0.00024186216,0.00054342893,0.00012360563,0.39292246],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9981427,0.00006314641,0.00045704836,0.0006454637,0.00025575527,0.0004358934],"domain_scores_gemma":[0.99847114,0.0001715548,0.0005341922,0.0005076116,0.00015535546,0.00016012102],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00013296973,0.00052681466,0.0007239363,0.00001466522,0.00028197753,0.000037045702,0.00038313642,0.0006241368,0.00035417167],"category_scores_gemma":[0.0000405157,0.0003447222,0.00071677106,0.000013927586,0.00097571,0.0000028581749,0.0005033627,0.0003218671,0.000055995646],"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":[0.00077001523,0.00075020775,0.019330297,0.0006795548,0.022272268,0.000073639494,0.00088846893,0.000034135235,0.2086946,0.10189694,0.36078012,0.28382975],"study_design_scores_gemma":[0.0008315802,0.0012606899,0.006739785,0.000041586132,0.00040112168,0.000020936573,0.00011176528,0.000059258535,0.0038294597,0.0017356521,0.98424953,0.0007186103],"about_ca_topic_score_codex":0.00004670772,"about_ca_topic_score_gemma":0.000005664807,"teacher_disagreement_score":0.6234694,"about_ca_system_score_codex":0.000024993034,"about_ca_system_score_gemma":0.000048700844,"threshold_uncertainty_score":0.99990046},"labels":[],"label_agreement":null},{"id":"W2325375091","doi":"10.1130/2008.2441(05)","title":"Carboniferous-Permian glaciation in the main Karoo Basin, South Africa: Stratigraphy, depositional controls, and glacial dynamics","year":2008,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":139,"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 Alberta; National Science Foundation","keywords":"Geology; Carboniferous; Paleontology; Diamictite; Gondwana; Foreland basin; Glacial period; Permian; Pennsylvanian; Structural basin; Deglaciation; Facies; Glacier; Geomorphology","score_opus":0.014936147745468028,"score_gpt":0.19038674086304894,"score_spread":0.1754505931175809,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2325375091","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.026686748,0.004867411,0.0003263736,0.00057878403,0.000085670225,0.0005877839,0.00064560404,0.00004468449,0.9661769],"genre_scores_gemma":[0.9962042,0.00038184196,0.001437639,0.00058721524,0.00011423548,0.000005868885,0.0001333885,0.0000029523164,0.0011326609],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979866,0.00015061209,0.0005108582,0.00047418792,0.00045667632,0.0004210713],"domain_scores_gemma":[0.99885255,0.00041309916,0.0003803616,0.00020099383,0.0000448702,0.000108152504],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00027919144,0.00038508675,0.0006568493,0.00006381471,0.00031668367,0.000032076638,0.00031697785,0.00065483386,0.00008871515],"category_scores_gemma":[0.000016552776,0.00027328968,0.00045538915,0.000053049054,0.0020980989,0.000048988284,0.0000065609743,0.0007596644,0.000002706686],"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":[0.0009232539,0.00016287823,0.52759004,0.00017318483,0.00091067975,0.0004002596,0.016935825,0.00012708748,0.000025528303,0.039105184,0.002778979,0.41086712],"study_design_scores_gemma":[0.00066780654,0.0007302135,0.9740472,0.000041359115,0.00009990527,0.00009870579,0.0011461751,0.0017577158,8.182821e-7,0.018706914,0.0022266898,0.00047652537],"about_ca_topic_score_codex":0.00053748663,"about_ca_topic_score_gemma":0.0017835586,"teacher_disagreement_score":0.96951747,"about_ca_system_score_codex":0.00000918893,"about_ca_system_score_gemma":0.00009937282,"threshold_uncertainty_score":0.9999719},"labels":[],"label_agreement":null},{"id":"W2325964117","doi":"10.1130/2008.2436(14)","title":"Tectonic architecture of an arc-arc collision zone, Newfoundland Appalachians","year":2008,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":56,"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; Ordovician; Island arc; Unconformity; Paleontology; Volcanic arc; Collision zone; Terrane; Forearc; Detritus; Basement; Subduction; Fibrous joint; Geochemistry; Tectonics; Archaeology; Geography","score_opus":0.012403010440849052,"score_gpt":0.1910561247345258,"score_spread":0.17865311429367675,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2325964117","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.13691726,0.0018532686,0.0011973577,0.00055178284,0.00009787632,0.0005922353,0.00053932355,0.00015920852,0.8580917],"genre_scores_gemma":[0.841824,0.0023224573,0.031584475,0.0024363818,0.00042703815,0.0000066437933,0.001462292,0.000030430629,0.11990626],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99703723,0.000080845464,0.0007729749,0.00080731674,0.0007292429,0.00057239743],"domain_scores_gemma":[0.9979416,0.0003909259,0.00066719105,0.0005035786,0.00014672143,0.0003499472],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00017382157,0.00056517887,0.0013824697,0.00007135538,0.00021103486,0.000014628265,0.0007005211,0.0007503407,0.0086852675],"category_scores_gemma":[0.000034901008,0.0003719529,0.0012175242,0.00010189753,0.0027042143,0.000031492913,0.00011676657,0.0009359377,0.000078083845],"study_design_candidate":"design_other","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":[0.0012874585,0.0005341688,0.057874568,0.0006478832,0.0021771314,0.00019321694,0.0021513149,0.01650391,0.0012107968,0.0014168619,0.005706992,0.9102957],"study_design_scores_gemma":[0.0024925955,0.010533597,0.09290909,0.0003966397,0.0011622414,0.00031272028,0.00053214136,0.010066243,0.00052829646,0.18409179,0.6930953,0.0038793306],"about_ca_topic_score_codex":0.004826773,"about_ca_topic_score_gemma":0.0008490515,"teacher_disagreement_score":0.90641636,"about_ca_system_score_codex":0.000010643092,"about_ca_system_score_gemma":0.00007914768,"threshold_uncertainty_score":0.9998732},"labels":[],"label_agreement":null},{"id":"W2335663341","doi":"10.1130/2011.2483(15)","title":"Travertine and tufa from Dalhousie Springs (Australia)—Implications for recognizing Martian springs","year":2011,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":9,"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; Tufa; Mars Exploration Program; Spring (device); Facies; Sedimentary depositional environment; Landform; Diagenesis; Martian; Earth science; Carbonate; Natural (archaeology); Volcano; Geochemistry; Hot spring; Geomorphology; Paleontology; Astrobiology","score_opus":0.06440175218275276,"score_gpt":0.2425744166274629,"score_spread":0.17817266444471014,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2335663341","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.11727381,0.0002919099,0.08304753,0.0029618992,0.00035391434,0.0029517729,0.002858962,0.00030557098,0.7899546],"genre_scores_gemma":[0.7845297,0.00014046657,0.06533268,0.0015299135,0.00085120345,0.00013309838,0.002549976,0.00007415247,0.14485885],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9987919,0.000007529889,0.0003552633,0.00046823628,0.00009928238,0.00027783887],"domain_scores_gemma":[0.99914575,0.00009694214,0.00035361273,0.00022128884,0.00006308465,0.00011931088],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008570062,0.00026013475,0.00042007276,0.000019155823,0.00015581417,0.000023984789,0.00020445173,0.00017153533,0.00044024354],"category_scores_gemma":[0.0000034723796,0.00023245912,0.0002862913,0.000014467261,0.00046287203,0.00006991723,0.000089272486,0.00023281535,0.000047924957],"study_design_candidate":"design_other","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":[0.0001777096,0.00017619354,0.026335645,0.00014133874,0.0012140896,0.0000017106614,0.005172498,0.0000279821,0.011915114,0.15968105,0.016215805,0.77894086],"study_design_scores_gemma":[0.00070902065,0.0005185537,0.03355879,0.00014287386,0.00035964325,0.0000016305428,0.00039829302,0.00026419119,0.00078961934,0.3970883,0.5651132,0.001055895],"about_ca_topic_score_codex":0.00066975725,"about_ca_topic_score_gemma":0.0000045021284,"teacher_disagreement_score":0.77788496,"about_ca_system_score_codex":0.000008640585,"about_ca_system_score_gemma":0.000023893022,"threshold_uncertainty_score":0.94794077},"labels":[],"label_agreement":null},{"id":"W2336008351","doi":"10.1130/2006.1198(08)","title":"Evidence from sulfur isotope and trace elements in pyrites for their multiple post-depositional processes in uranium ores at the Stanleigh Mine, Elliot Lake, Ontario, Canada","year":2006,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","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":"NASA Astrobiology Institute","keywords":"Pyrite; δ34S; Electron microprobe; Troilite; Geology; Sulfur; Mineralogy; Geochemistry; Sedimentary depositional environment; Trace element; Quartz; Metallurgy; Meteorite; Materials science; Geomorphology; Chondrite; Structural basin","score_opus":0.016784782004505932,"score_gpt":0.18305281201125226,"score_spread":0.16626803000674634,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2336008351","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96546954,0.006158629,0.000025703735,0.0020931636,0.00003997601,0.0008720245,0.0030166241,0.000020830814,0.022303523],"genre_scores_gemma":[0.96759045,0.0005199611,0.0017855003,0.0017887655,0.000076113145,0.000027123035,0.0019396622,0.000007790916,0.026264653],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978917,0.000043235512,0.0006172655,0.000617706,0.0003903843,0.00043968583],"domain_scores_gemma":[0.99676955,0.0024928176,0.00031921448,0.00016431023,0.0001485728,0.00010550831],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00016952372,0.0003798505,0.00067784445,0.000025853198,0.00015523638,0.000026102716,0.00036054972,0.0002597065,0.0052084397],"category_scores_gemma":[0.00011080512,0.00021970371,0.0002364232,0.00006517798,0.00071348174,0.00004482075,0.00011247765,0.00040346844,0.000002917367],"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":[0.00048582448,0.00005826856,0.9816069,0.00014703105,0.00017479836,0.000021801225,0.00056238536,0.0011764427,0.00026531314,0.000015983165,0.0046960525,0.010789187],"study_design_scores_gemma":[0.00084780034,0.00063819735,0.91631,0.00031499774,0.00012944454,0.000007136554,0.0003956116,0.0019182494,0.0003952528,0.017984565,0.060216777,0.0008419593],"about_ca_topic_score_codex":0.88973284,"about_ca_topic_score_gemma":0.9961506,"teacher_disagreement_score":0.10641776,"about_ca_system_score_codex":0.00004293648,"about_ca_system_score_gemma":0.0002484673,"threshold_uncertainty_score":0.99570096},"labels":[],"label_agreement":null},{"id":"W2336913291","doi":"10.1130/2012.2486(10)","title":"The importance of spatial thinking for geoscience education: Insights from the crossroads of geoscience and cognitive science","year":2012,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geography Education and Pedagogy","field":"Social Sciences","cited_by":71,"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":"","keywords":"Earth science; Curriculum; Geologist; Field (mathematics); Cognition; Spatial cognition; Perspective (graphical); Cognitive map; Perception; Variety (cybernetics); Computer science; Data science; Psychology; Geography; Geology; Archaeology; Artificial intelligence; Pedagogy","score_opus":0.034519496539993325,"score_gpt":0.3217050998349518,"score_spread":0.2871856032949585,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2336913291","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.27732846,0.03150778,0.013668191,0.009468268,0.0037996355,0.005609024,0.00051288685,0.00012312461,0.65798265],"genre_scores_gemma":[0.9703779,0.0015585311,0.004863646,0.0019876421,0.00044415545,0.0000649293,0.00001259185,0.0000124658845,0.020678109],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99762654,0.00007459339,0.000510298,0.00046623586,0.00090512604,0.00041717588],"domain_scores_gemma":[0.99538106,0.0020685988,0.001186516,0.00032232123,0.00089098135,0.0001505023],"candidate_categories":["sts"],"consensus_categories":["sts"],"category_scores_codex":[0.0012567545,0.00020950456,0.00039042614,0.000035151465,0.0020381024,0.000070874645,0.001123392,0.00021260545,0.00009553067],"category_scores_gemma":[0.00050439505,0.00012661876,0.0003024423,0.00012637836,0.03149364,0.00010631085,0.00025856242,0.00027141054,0.0000010519526],"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":[0.00005973108,0.00012872495,0.034295894,0.000044956952,0.000092796974,9.233666e-8,0.070646666,5.803118e-7,0.00022610376,0.4088315,0.00031047742,0.48536247],"study_design_scores_gemma":[0.0004285237,0.00052115583,0.17475529,0.00034269024,0.0002873961,0.0000019975346,0.07521546,0.00006905104,0.00023698516,0.27993077,0.46747756,0.0007331292],"about_ca_topic_score_codex":0.005602737,"about_ca_topic_score_gemma":0.0003822288,"teacher_disagreement_score":0.6930495,"about_ca_system_score_codex":0.000032244818,"about_ca_system_score_gemma":0.0017126203,"threshold_uncertainty_score":0.9992611},"labels":[],"label_agreement":null},{"id":"W2337587523","doi":"10.1130/0-8137-2352-3.341","title":"Archean mantle plumes: Evidence from greenstone belt geochemistry","year":2001,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":89,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Laurentian University; Geological Survey of Canada","funders":"University of Portsmouth; National Science Foundation","keywords":"Greenstone belt; Archean; Geology; Geochemistry; Mantle plume; Mantle (geology); Seismology; Tectonics; Lithosphere","score_opus":0.029526137239677827,"score_gpt":0.21098125124791683,"score_spread":0.181455114008239,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2337587523","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.07405973,0.0038627994,0.00035368808,0.0011350628,0.000080321726,0.0002595958,0.00048782767,0.0001678066,0.91959316],"genre_scores_gemma":[0.6122936,0.005708885,0.015900575,0.004730101,0.0009370487,0.000008001289,0.00232723,0.000028760045,0.3580658],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9966952,0.000047977992,0.00075297564,0.0010626662,0.00075086905,0.00069031416],"domain_scores_gemma":[0.9974305,0.00085242133,0.0005799576,0.00059038063,0.00014639951,0.00040035383],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001984918,0.00063464197,0.0012531872,0.000030589497,0.0001893,0.000027264708,0.00086259085,0.00073628523,0.06479664],"category_scores_gemma":[0.000092542774,0.0004596338,0.0012889154,0.00006824212,0.002361301,0.000045745455,0.00020754551,0.0010396168,0.0005116849],"study_design_candidate":"design_other","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":[0.0004783556,0.00016277104,0.12765588,0.00035579063,0.0022041614,0.0003092165,0.0006949774,0.00039892626,0.0026054732,0.00033664415,0.029830223,0.83496755],"study_design_scores_gemma":[0.0011441348,0.0019609376,0.13672037,0.0012847469,0.0017370712,0.000089939334,0.00075879495,0.007383524,0.0016040207,0.5615182,0.28121206,0.0045861956],"about_ca_topic_score_codex":0.0146384165,"about_ca_topic_score_gemma":0.00042066406,"teacher_disagreement_score":0.8303814,"about_ca_system_score_codex":0.000014667777,"about_ca_system_score_gemma":0.000057848454,"threshold_uncertainty_score":0.99978554},"labels":[],"label_agreement":null},{"id":"W2339799416","doi":"10.1130/0-8137-1197-5.243","title":"SHRIMP U-Pb zircon geochronology of the Bondy gneiss complex: Evidence for circa 1.39 Ga arc magmatism and polyphase Grenvillian metamorphism in the Central Metasedimentary Belt, Grenville Province, Québec","year":2004,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":22,"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":"Zircon; Gneiss; Geology; Geochemistry; Protolith; Metamorphism; Archean; Geochronology; Petrology; Metamorphic rock","score_opus":0.03493169370249237,"score_gpt":0.22430089487087188,"score_spread":0.18936920116837952,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2339799416","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5844312,0.08165837,0.0043265335,0.093358144,0.0009282782,0.01585028,0.0074505876,0.00031659452,0.21168007],"genre_scores_gemma":[0.98160416,0.0005985218,0.0068072467,0.0069585186,0.00011607434,0.000026581227,0.00033227194,0.000012359871,0.0035442377],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99696654,0.00016752882,0.00088323484,0.00075770105,0.0005087002,0.0007162975],"domain_scores_gemma":[0.9973869,0.001113234,0.0007536541,0.0005044698,0.00006763459,0.00017414706],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004193715,0.00053317996,0.0012151517,0.00005327311,0.00026477897,0.000020028261,0.0009638377,0.0004013945,0.0043137097],"category_scores_gemma":[0.0000873253,0.0002837988,0.00102002,0.00009095263,0.0041141133,0.000050276136,0.00019091097,0.0006584638,0.000009976374],"study_design_candidate":"design_other","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":[0.002601395,0.0015746763,0.16261703,0.0035756005,0.0069073257,0.00024964317,0.0064341445,0.003305901,0.022896182,0.047942147,0.017619563,0.7242764],"study_design_scores_gemma":[0.004389859,0.005533193,0.49161154,0.0007905699,0.003443061,0.00017983779,0.0013400384,0.0031116756,0.0019005279,0.3623952,0.12262645,0.0026780388],"about_ca_topic_score_codex":0.06828052,"about_ca_topic_score_gemma":0.015085455,"teacher_disagreement_score":0.7215983,"about_ca_system_score_codex":0.000033495984,"about_ca_system_score_gemma":0.00022157704,"threshold_uncertainty_score":0.99996144},"labels":[],"label_agreement":null},{"id":"W2340769242","doi":"10.1130/0-8137-1197-5.65","title":"Mesoproterozoic basement of the Lac St. Jean Anorthosite Suite and younger Grenvillian intrusions in the Saguenay region, Québec: Structural relationships and U-Pb geochronology","year":2004,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":28,"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":"Anorthosite; Gneiss; Geology; Geochronology; Geochemistry; Basement; Suite; Metamorphic rock; Paleontology; Geography; Archaeology; Plagioclase","score_opus":0.017300371899078938,"score_gpt":0.1856943608784517,"score_spread":0.16839398897937277,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2340769242","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.92496234,0.0055687516,0.00009728369,0.0262585,0.00008628992,0.0012916273,0.00023411507,0.00004642597,0.041454658],"genre_scores_gemma":[0.99217033,0.00047149087,0.00056956976,0.0016317328,0.000043906613,0.000004965015,0.00009557493,0.0000043106547,0.005008111],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981625,0.00017714353,0.0005411973,0.0004779224,0.00031345128,0.0003277989],"domain_scores_gemma":[0.9985068,0.000551437,0.00044241213,0.00033927325,0.00006126296,0.00009881698],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00027186843,0.00032314958,0.0005949788,0.000037179354,0.00031174274,0.00001643507,0.00038811885,0.0003740747,0.0017014357],"category_scores_gemma":[0.000082624,0.00015828817,0.00030976743,0.00008637566,0.0028990402,0.000036675156,0.00016384326,0.00082716084,0.0000043732516],"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":[0.000088542794,0.000032223437,0.949251,0.0001244435,0.0003058114,0.000018050372,0.0020170219,0.00045701533,0.000050035895,0.00590662,0.00075904524,0.040990207],"study_design_scores_gemma":[0.00039961748,0.00041136006,0.8472566,0.000091818314,0.00023188636,0.000033010983,0.00048455037,0.00043121463,0.000015091258,0.13701606,0.013243554,0.0003852272],"about_ca_topic_score_codex":0.03497065,"about_ca_topic_score_gemma":0.021543749,"teacher_disagreement_score":0.13110943,"about_ca_system_score_codex":0.000011791546,"about_ca_system_score_gemma":0.00005788994,"threshold_uncertainty_score":0.9998145},"labels":[],"label_agreement":null},{"id":"W2341268128","doi":"10.1130/2010.2465(16)","title":"Debrisites from the Sudbury impact event in Ontario, north of Lake Superior, and a new age constraint: Are they base-surge deposits or tsunami deposits?","year":2010,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","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":"","keywords":"Ejecta; Lapilli; Geology; Impact crater; Bay; Geochemistry; Impact structure; Breccia; Seismology; Pyroclastic rock; Oceanography; Volcano","score_opus":0.02381480769527573,"score_gpt":0.21629136631737245,"score_spread":0.19247655862209673,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2341268128","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9892139,0.00011885711,0.0007848042,0.00016029789,0.00005131562,0.00045874066,0.0004434888,0.00001793918,0.008750664],"genre_scores_gemma":[0.992908,0.00003444054,0.0016055604,0.000337532,0.00008502269,0.0000069744533,0.00077311357,0.000013260248,0.0042361105],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985544,0.000037034868,0.00045900032,0.0003943258,0.00025607995,0.00029917524],"domain_scores_gemma":[0.9987608,0.00033971237,0.00043696084,0.00027451184,0.00004312385,0.00014488061],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011280672,0.00034658558,0.00069133023,0.000020607971,0.00011542291,0.00003505324,0.00028467417,0.0002180858,0.0007155056],"category_scores_gemma":[0.000007192105,0.00020603953,0.00038893826,0.000024721465,0.00068114384,0.00006852378,0.00012770928,0.0007030356,0.000007722776],"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":[0.00013348488,0.00006638894,0.9659871,0.000014058745,0.00032917663,0.00002655775,0.0041564694,0.00010468249,0.0008886507,0.00025014204,0.00052693696,0.027516345],"study_design_scores_gemma":[0.0007398543,0.00052463496,0.98010343,0.00024347244,0.00018565424,0.000008815539,0.0011827277,0.00020643424,0.00016243587,0.007832216,0.0081734955,0.0006368448],"about_ca_topic_score_codex":0.08310666,"about_ca_topic_score_gemma":0.27327827,"teacher_disagreement_score":0.1901716,"about_ca_system_score_codex":0.000023524153,"about_ca_system_score_gemma":0.0002578155,"threshold_uncertainty_score":0.922999},"labels":[],"label_agreement":null},{"id":"W2342462444","doi":"10.1130/2014.0038(05)","title":"Multiple Younger Dryas and Allerød moraines (Sumas Stade) and late Pleistocene Everson glaciomarine drift in the Fraser Lowland","year":2014,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geology and Paleoclimatology Research","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":"","keywords":"Geology; Deglaciation; Bedrock; Glacial period; Pleistocene; Younger Dryas; Geomorphology; Paleontology; Earth science; Archaeology; Geography","score_opus":0.02065317339218445,"score_gpt":0.2163198269507625,"score_spread":0.19566665355857804,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2342462444","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7888221,0.0029166883,0.000077386525,0.0028492333,0.0001099244,0.0008906721,0.00010294841,0.00005457835,0.20417644],"genre_scores_gemma":[0.95524216,0.0010978674,0.00067989307,0.0019504232,0.000071297465,0.0000057400425,0.0001635696,0.000008371025,0.040780686],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981678,0.00013776137,0.00036169903,0.0005471327,0.00029656544,0.0004890023],"domain_scores_gemma":[0.9981466,0.0011890203,0.00021622116,0.00026775984,0.000052062824,0.00012832216],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005854184,0.00035999512,0.0007101616,0.00005358041,0.0002299376,0.000024231866,0.00032118903,0.00065781747,0.0009424894],"category_scores_gemma":[0.00005583347,0.00022863083,0.0001660627,0.00003208093,0.0028834813,0.0000353362,0.00010514603,0.0008542625,0.000036734597],"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":[0.00020810055,0.0000115001485,0.9895237,0.00008979762,0.00011270786,0.000039671162,0.00096927193,0.000023011184,0.0000028845225,0.00037948575,0.000590885,0.008048973],"study_design_scores_gemma":[0.0014189223,0.00094200973,0.92156005,0.000059380272,0.00007848839,0.00006240313,0.0004968538,0.0044891275,0.0000023869623,0.007894578,0.062453657,0.00054212456],"about_ca_topic_score_codex":0.0014939421,"about_ca_topic_score_gemma":0.0017470384,"teacher_disagreement_score":0.16642003,"about_ca_system_score_codex":0.0000018225402,"about_ca_system_score_gemma":0.000030397452,"threshold_uncertainty_score":0.9999708},"labels":[],"label_agreement":null},{"id":"W2343096805","doi":"10.1130/2014.0038(06)","title":"The life and times of the Cordilleran Ice Sheet around the southern Fraser Plateau, British Columbia","year":2014,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geology and Paleoclimatology Research","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":"University of the Fraser Valley; Simon Fraser University","funders":"","keywords":"Bedrock; Geology; Deglaciation; Glacial period; Natural (archaeology); Plateau (mathematics); Earth science; Ice sheet; Geomorphology; Archaeology; Physical geography; Paleontology; Geography","score_opus":0.01375431105439391,"score_gpt":0.19689372027780058,"score_spread":0.18313940922340669,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2343096805","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.16399543,0.005778387,0.000018742296,0.0030966655,0.00030273868,0.0009333912,0.00031921852,0.00004691292,0.82550853],"genre_scores_gemma":[0.7565913,0.0009788576,0.000099661214,0.0025230981,0.000119452896,0.000004802288,0.000032063825,0.000008992185,0.23964176],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9980989,0.0002698894,0.00042578837,0.00037719784,0.00038428346,0.00044393848],"domain_scores_gemma":[0.9967668,0.002132403,0.000437821,0.00044832425,0.000100917845,0.00011370628],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00068205263,0.0002185898,0.000583087,0.000006924903,0.0010648317,0.000080497375,0.00084572186,0.0005611306,0.004211937],"category_scores_gemma":[0.00010746938,0.0001309444,0.00040375162,0.000030664334,0.009675817,0.000012709277,0.0001729573,0.0009743492,0.000070505725],"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":[0.00007628885,0.000009150235,0.93981993,0.000059756458,0.00047405413,0.000005138925,0.00048484362,0.000050192317,7.356266e-7,0.00035155838,0.027570942,0.031097382],"study_design_scores_gemma":[0.0010648601,0.0010051605,0.4001437,0.00016637128,0.00033362847,0.00014561463,0.0037633548,0.0020175008,0.0000020727107,0.055382993,0.535164,0.0008107366],"about_ca_topic_score_codex":0.008528486,"about_ca_topic_score_gemma":0.013846686,"teacher_disagreement_score":0.5925959,"about_ca_system_score_codex":0.0000011778391,"about_ca_system_score_gemma":0.000092889044,"threshold_uncertainty_score":0.9980738},"labels":[],"label_agreement":null},{"id":"W2343288261","doi":"10.1130/0-8137-2343-4.23","title":"Yukon-Tanana Terrane in the Scotia-Quaal Belt, Coast Plutonic Complex, central-western British Columbia","year":2000,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Terrane; Geology; Devonian; Geochemistry; Lithology; Paleozoic; Zircon; Paleontology; Tectonics","score_opus":0.01843715378878061,"score_gpt":0.19028960013180954,"score_spread":0.17185244634302893,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2343288261","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.23169889,0.0017177407,0.00003775511,0.0013337769,0.00010197648,0.0008419215,0.0009257211,0.00013409654,0.7632081],"genre_scores_gemma":[0.9274216,0.0010873772,0.0008121738,0.0077905767,0.00021757302,0.000005086995,0.0012822298,0.000013656762,0.061369702],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99636096,0.00013545259,0.000893804,0.00086062425,0.00076936313,0.0009798069],"domain_scores_gemma":[0.998412,0.00041432888,0.0004154972,0.00043798986,0.00006010932,0.00026008504],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00027337566,0.00046075418,0.0012781342,0.000026085703,0.0002656202,0.00016193028,0.0010810428,0.0005944298,0.05541479],"category_scores_gemma":[0.000020307822,0.00039290008,0.001085643,0.000113393995,0.0024365159,0.0000429363,0.00010217288,0.0010930013,0.00017868323],"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":[0.00018881202,0.0003600725,0.41646188,0.00022718628,0.00087230373,0.00050884625,0.0013926065,0.0011444549,0.00003090346,0.00019773537,0.045441188,0.533174],"study_design_scores_gemma":[0.00091089297,0.0010581848,0.71224576,0.00021207088,0.00033243155,0.00015874486,0.0004929665,0.0014897133,0.0000017137056,0.06546576,0.216294,0.001337742],"about_ca_topic_score_codex":0.18303728,"about_ca_topic_score_gemma":0.20188554,"teacher_disagreement_score":0.70183843,"about_ca_system_score_codex":0.000015930258,"about_ca_system_score_gemma":0.000057266825,"threshold_uncertainty_score":0.9998523},"labels":[],"label_agreement":null},{"id":"W2344981234","doi":"10.1130/0-8137-2374-4.439","title":"The Quaternary Moctezuma volcanic field: A tholeiitic to alkali basaltic episode in the central Sonoran Basin and Range Province, Mexico","year":2003,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","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":"Saint Mary's University","funders":"Natural Sciences and Engineering Research Council of Canada; Universidad de Sonora","keywords":"Volcano; Basalt; Geology; Quaternary; Range (aeronautics); Geochemistry; Structural basin; Alkali metal; Field (mathematics); Earth science; Geomorphology; Paleontology; Chemistry; Materials science","score_opus":0.01192511791318956,"score_gpt":0.19509683335787403,"score_spread":0.18317171544468447,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2344981234","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.1529441,0.005759143,0.0007206558,0.05069449,0.0002822126,0.0026642785,0.0002679939,0.00013332866,0.7865338],"genre_scores_gemma":[0.9243896,0.001173607,0.0015823832,0.03232511,0.00015117547,0.000023122591,0.000063527186,0.000012744855,0.040278718],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9974526,0.00020313243,0.00055149995,0.0005945402,0.00046253682,0.0007356885],"domain_scores_gemma":[0.99772966,0.0013903265,0.00023817288,0.00037264868,0.000047397527,0.0002218223],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00046291164,0.000419728,0.0007075331,0.00003225146,0.0002971289,0.00006552642,0.00068272196,0.00034428728,0.0016330724],"category_scores_gemma":[0.00012187273,0.00020716885,0.0005087412,0.00008321163,0.0010946387,0.000028426522,0.00009501404,0.0007151781,0.00005010099],"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":[0.0007579379,0.00023249473,0.46135238,0.00033339864,0.0009984927,0.00025337617,0.0029618475,0.0005557184,0.000054129905,0.010375079,0.04213295,0.47999218],"study_design_scores_gemma":[0.0010657498,0.0031247388,0.16214669,0.00025804955,0.0005411536,0.00008342171,0.0019689212,0.0060767187,0.00005018181,0.22263262,0.6003001,0.0017516986],"about_ca_topic_score_codex":0.0059540602,"about_ca_topic_score_gemma":0.0027066863,"teacher_disagreement_score":0.7714455,"about_ca_system_score_codex":0.000010963592,"about_ca_system_score_gemma":0.000037052534,"threshold_uncertainty_score":0.99927956},"labels":[],"label_agreement":null},{"id":"W2349259843","doi":"10.1130/2014.0038(07)","title":"Quaternary subglacial and explosive volcanism in the Canadian Cascade arc (Sea-to-Sky Corridor), British Columbia","year":2014,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geology and Paleoclimatology Research","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":"Bedrock; Geology; Deglaciation; Glacial period; Natural (archaeology); Earth science; Quaternary; Volcanism; Geomorphology; Paleontology; Tectonics","score_opus":0.021156082860898238,"score_gpt":0.21304606567151468,"score_spread":0.19188998281061645,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2349259843","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.36580807,0.00087601173,0.00002751753,0.0030525085,0.00024177763,0.0012968448,0.00032582672,0.00004532664,0.6283261],"genre_scores_gemma":[0.9251575,0.00032378465,0.00045656358,0.0102848625,0.00015317895,0.000014699769,0.00019658662,0.000010245224,0.0634026],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9976085,0.0002227658,0.00039922787,0.00059764966,0.00038703447,0.00078485993],"domain_scores_gemma":[0.99849683,0.0005827411,0.00017452691,0.00027481274,0.00007966644,0.00039141488],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00056449,0.0002626295,0.0006972489,0.000053610816,0.000516043,0.000104153994,0.0006413753,0.000833197,0.0026689814],"category_scores_gemma":[0.000056786983,0.00026182123,0.00022671581,0.000045088054,0.0026459983,0.000021789345,0.0000698181,0.0011888943,0.00018589913],"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":[0.000026930213,0.00000568197,0.9739379,0.00003425232,0.000056487766,0.00023254707,0.0008170791,0.000009761762,5.1214e-7,0.00015741267,0.012933932,0.011787474],"study_design_scores_gemma":[0.0005202146,0.001125829,0.8017674,0.0001125951,0.00006163107,0.00056477194,0.0005633048,0.0004702004,0.0000011153411,0.016089786,0.17803922,0.000683919],"about_ca_topic_score_codex":0.64007753,"about_ca_topic_score_gemma":0.9589848,"teacher_disagreement_score":0.5649235,"about_ca_system_score_codex":0.000009458216,"about_ca_system_score_gemma":0.00023470334,"threshold_uncertainty_score":0.9999834},"labels":[],"label_agreement":null},{"id":"W2353250242","doi":"10.1130/2011.0024(03)","title":"Geology and geochronology of Paleoarchean gneisses in the Minnesota River Valley","year":2011,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":"","keywords":"Gneiss; Geology; Metamorphism; Geochemistry; Granulite; Geochronology; Metamorphic facies; Archean; Outcrop; Migmatite; Intrusion; Facies; Archaeology; Metamorphic rock; Geomorphology; Geography","score_opus":0.023808044441294172,"score_gpt":0.19479486586373065,"score_spread":0.17098682142243649,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2353250242","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.2051718,0.0044257725,0.00007869599,0.0013600666,0.000048145135,0.00039931358,0.00008365813,0.00003431006,0.78839827],"genre_scores_gemma":[0.98030305,0.0024950623,0.0027908522,0.0018184603,0.00006953432,0.0000042576453,0.00011929122,0.000005807087,0.012393702],"study_design_codex":"observational","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9979786,0.00012817005,0.00062115904,0.00055502745,0.00025604543,0.00046097746],"domain_scores_gemma":[0.9982602,0.0007788246,0.00044442405,0.00033412932,0.00008026146,0.00010213531],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003108148,0.00036822498,0.0010253389,0.000057431338,0.00007854185,0.0000048724455,0.00060844305,0.00061383087,0.009775968],"category_scores_gemma":[0.000052951775,0.00021115976,0.00049987924,0.000057467798,0.0058837202,0.00002193353,0.00014043142,0.0006480049,0.000044213193],"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":[0.0004438779,0.00025454286,0.531309,0.0004607892,0.0010788784,0.000111971895,0.0049017775,0.00009965356,0.00015385397,0.029961752,0.0027745548,0.42844936],"study_design_scores_gemma":[0.000559263,0.0018999244,0.33412904,0.0000540552,0.0002683819,0.00005837928,0.00061770366,0.00032709114,0.000038036163,0.609392,0.051990848,0.00066526997],"about_ca_topic_score_codex":0.004786527,"about_ca_topic_score_gemma":0.0004572211,"teacher_disagreement_score":0.77600455,"about_ca_system_score_codex":0.0000029154257,"about_ca_system_score_gemma":0.000031236395,"threshold_uncertainty_score":0.9968217},"labels":[],"label_agreement":null},{"id":"W2354973351","doi":"10.1130/0-8137-1197-5.81","title":"Low-variance sapphirine-bearing assemblages from Wilson Lake, Grenville Province of Labrador","year":2004,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","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":"","keywords":"Granulite; Geology; Sillimanite; Geochemistry; Gneiss; Metamorphism; Anorthosite; Plagioclase; Massif; Kyanite; Pelite; Metamorphic rock; Biotite; Geomorphology; Facies; Quartz; Paleontology","score_opus":0.012275486980463485,"score_gpt":0.18490419806274797,"score_spread":0.17262871108228448,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2354973351","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.1581903,0.0022122809,0.0008206644,0.0009178245,0.00015917503,0.00063182676,0.0010763976,0.00017668404,0.83581483],"genre_scores_gemma":[0.92536074,0.0007651187,0.012275,0.0012745397,0.00027597306,0.0000037750478,0.0006333463,0.000017113636,0.059394423],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9971966,0.000042641994,0.0007848407,0.00083903316,0.0006191211,0.00051776116],"domain_scores_gemma":[0.9980074,0.00039181588,0.0008023126,0.00044296356,0.00012689088,0.00022862805],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00015352604,0.00053308957,0.0013231313,0.000037040063,0.00012088476,0.000019958447,0.00067158387,0.0006428536,0.019295558],"category_scores_gemma":[0.000052263385,0.00038075916,0.0009858123,0.00007130338,0.0016048214,0.000040456216,0.00017747137,0.00070122926,0.00014030641],"study_design_candidate":"design_other","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":[0.0010162255,0.00077606615,0.092337206,0.0019644757,0.0046802657,0.00037673567,0.0012768406,0.011164782,0.00863961,0.016971378,0.0057929223,0.8550035],"study_design_scores_gemma":[0.002734694,0.0036126168,0.17117459,0.0016994561,0.0013980899,0.000021766375,0.0005271631,0.0035955475,0.008795632,0.643486,0.1585974,0.0043570297],"about_ca_topic_score_codex":0.005283193,"about_ca_topic_score_gemma":0.000955378,"teacher_disagreement_score":0.85064644,"about_ca_system_score_codex":0.000011017755,"about_ca_system_score_gemma":0.0000953695,"threshold_uncertainty_score":0.99986446},"labels":[],"label_agreement":null},{"id":"W2382762531","doi":"10.1130/2010.1206(15)","title":"Lithochemistry of the Lower Paleozoic Goldenville and Halifax groups, southwestern Nova Scotia, Canada: Implications for stratigraphy, provenance, and tectonic setting of the Meguma terrane","year":2010,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological formations and processes","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":true,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; Acadia University; Geological Society of America","keywords":"Geology; Felsic; Provenance; Geochemistry; Terrane; Petrography; Craton; Clastic rock; Mafic; Paleontology; Sedimentary rock; Tectonics","score_opus":0.01107661601630906,"score_gpt":0.19012329485593213,"score_spread":0.17904667883962308,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2382762531","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.86010593,0.0031442433,0.00021869289,0.0025549012,0.00023038729,0.0018459979,0.0031403461,0.000029736822,0.12872973],"genre_scores_gemma":[0.9962572,0.00006901139,0.0016558105,0.00025943833,0.000027881468,0.000004249294,0.000038625978,0.000003927933,0.0016838893],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99890053,0.000012696048,0.00042573968,0.00026433592,0.00018405351,0.00021266333],"domain_scores_gemma":[0.9986799,0.00022893325,0.00062407565,0.00029037116,0.00011583532,0.00006091832],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012411161,0.00021544367,0.00041276822,0.000009490207,0.0001976069,0.00001222929,0.0003534894,0.00027313322,0.00015035154],"category_scores_gemma":[0.000030209225,0.00011356824,0.00023566005,0.000044746743,0.0015343976,0.000022755416,0.00007751467,0.0003441474,2.0623682e-7],"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":[0.00012365244,0.00009733374,0.8755536,0.0029187691,0.00056155835,5.676535e-7,0.0014196514,0.00010689626,0.0029104194,0.008096567,0.0011374641,0.10707354],"study_design_scores_gemma":[0.0004717288,0.00048691308,0.95280534,0.00030221615,0.00020821116,0.000033320768,0.0005627713,0.00015308532,0.00073784025,0.03086205,0.012887091,0.00048942043],"about_ca_topic_score_codex":0.029084789,"about_ca_topic_score_gemma":0.08166196,"teacher_disagreement_score":0.13615121,"about_ca_system_score_codex":0.0000028336726,"about_ca_system_score_gemma":0.00016027033,"threshold_uncertainty_score":0.97738063},"labels":[],"label_agreement":null},{"id":"W2395810804","doi":"10.1130/2014.0037(04)","title":"Tracking a big Miocene river across the Continental Divide at Monida Pass, Montana/Idaho","year":2014,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geology and Paleoclimatology Research","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":"Geology; Tectonics; Precambrian; Paleontology; Orogeny; Earth science; Archaeology; Geography","score_opus":0.03089277722763831,"score_gpt":0.23893752285157135,"score_spread":0.20804474562393305,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2395810804","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.32307875,0.004875918,0.00037548775,0.0034309677,0.0005824381,0.0010545834,0.00048833835,0.00018422813,0.6659293],"genre_scores_gemma":[0.85250574,0.0005416398,0.00038983917,0.0023391936,0.00023541841,0.000006261358,0.00021138041,0.000013261062,0.14375728],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99696225,0.00019743615,0.0005823583,0.0007248824,0.000551511,0.000981543],"domain_scores_gemma":[0.99735814,0.001273917,0.0005208602,0.000513371,0.00012008,0.00021362008],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006402386,0.00051426515,0.0010001858,0.000025595238,0.0008450084,0.000031643176,0.0008581666,0.000986084,0.0023178807],"category_scores_gemma":[0.000060018607,0.00032303255,0.0008589238,0.000038236427,0.0067589525,0.00002472613,0.00027494325,0.0012567515,0.00047213925],"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":[0.00019823248,0.00001539757,0.92357,0.00006431234,0.0004638029,0.000055520533,0.0011242199,0.00005825904,0.000008540698,0.00041375565,0.00474581,0.06928219],"study_design_scores_gemma":[0.0010174447,0.00090829463,0.6340643,0.000107474305,0.00021962401,0.00023520675,0.00038269436,0.00084159296,0.000054353368,0.0116050085,0.34958628,0.0009777341],"about_ca_topic_score_codex":0.0009639645,"about_ca_topic_score_gemma":0.00095848576,"teacher_disagreement_score":0.529427,"about_ca_system_score_codex":0.000008131568,"about_ca_system_score_gemma":0.000051474206,"threshold_uncertainty_score":0.99992216},"labels":[],"label_agreement":null},{"id":"W2395851439","doi":"10.1130/2006.2405(05)","title":"Relicts of Earth's earliest crust: U-Pb, Lu-Hf, and morphological characteristics of &amp;gt;3.7 Ga detrital zircon of the western Canadian Shield","year":2006,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","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":true,"ca_institutions":"","funders":"Manitoba Hydro","keywords":"Zircon; Geology; Detritus; Geochemistry; Hadean; Crust; Shield; Paleontology","score_opus":0.015718194860039537,"score_gpt":0.1788893616385748,"score_spread":0.16317116677853527,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2395851439","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7535834,0.0009974375,0.0001229964,0.0008204815,0.00010966243,0.00045659512,0.0014874556,0.000030060091,0.24239194],"genre_scores_gemma":[0.9754606,0.00031386066,0.0024202066,0.0008129431,0.00007547702,0.0000015503304,0.00020907838,0.000007703499,0.020698572],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9973568,0.000072954084,0.0010178249,0.0005213342,0.0005395273,0.0004915964],"domain_scores_gemma":[0.997602,0.00047966512,0.0010080088,0.00042634993,0.00020735065,0.00027661084],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00022863265,0.00042798193,0.0013999243,0.00006527887,0.0001133519,0.000011623656,0.00058476115,0.00079515344,0.003012593],"category_scores_gemma":[0.00012849439,0.00026335183,0.00083530345,0.0001035552,0.003718704,0.000025963538,0.00017056448,0.00064769463,0.000015769385],"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":[0.0003452188,0.0002569184,0.90923643,0.0007907276,0.0009670385,0.00006522042,0.0007292916,0.00027984564,0.011413544,0.001274448,0.004775132,0.069866166],"study_design_scores_gemma":[0.0006775385,0.0016573808,0.9165077,0.00033279607,0.0006155937,0.000058451267,0.00018424694,0.00016317847,0.002489465,0.0104583595,0.065786175,0.0010691215],"about_ca_topic_score_codex":0.060847998,"about_ca_topic_score_gemma":0.007874522,"teacher_disagreement_score":0.22187725,"about_ca_system_score_codex":0.000005803487,"about_ca_system_score_gemma":0.00009177894,"threshold_uncertainty_score":0.9999819},"labels":[],"label_agreement":null},{"id":"W2410502332","doi":"10.1130/2011.0024(26)","title":"Interpreting origins of landform sediment assemblages within the Upper Mississippi River Valley and tributaries in the Twin Cities area of Minnesota","year":2011,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Archaeology and Natural History","field":"Social 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":"","keywords":"Tributary; Geology; Precambrian; Landform; Archaeology; Hydrology (agriculture); Geomorphology; Paleontology; Geography; Cartography","score_opus":0.02831802685257041,"score_gpt":0.2531263680267686,"score_spread":0.22480834117419818,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2410502332","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.20208633,0.011664978,0.0001767552,0.0053797746,0.00033613696,0.0013245542,0.00008548507,0.00006133715,0.77888465],"genre_scores_gemma":[0.96558595,0.0022195608,0.0016563525,0.0012608882,0.00007018362,0.000017588995,0.00000884611,0.000012564578,0.029168097],"study_design_codex":"qualitative","study_design_gemma":"not_applicable","domain_scores_codex":[0.9984349,0.00021026187,0.00048287265,0.00024880387,0.00037103795,0.0002521043],"domain_scores_gemma":[0.9979173,0.0010676314,0.0006583989,0.00020460042,0.00010602132,0.00004605759],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.0010222998,0.00023110583,0.0006119191,0.000036093243,0.00030102849,0.0000023389614,0.00053303887,0.0004652627,0.00020097155],"category_scores_gemma":[0.00011934728,0.00012397465,0.00033242386,0.000033111144,0.01252769,0.000036732974,0.00024498298,0.00061366445,0.0000010039286],"study_design_candidate":"qualitative","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":[0.0003522124,0.0000793435,0.01052573,0.00016021282,0.00047019048,0.000008625802,0.65596884,0.000002874053,0.000092839146,0.3082288,0.0057093664,0.01840098],"study_design_scores_gemma":[0.0006419686,0.0010905591,0.009373716,0.0005514049,0.00031865097,0.000007916334,0.05723985,0.00003205378,0.00023468056,0.25316322,0.67669535,0.0006506353],"about_ca_topic_score_codex":0.0032614914,"about_ca_topic_score_gemma":0.00020272854,"teacher_disagreement_score":0.76349956,"about_ca_system_score_codex":0.00007625773,"about_ca_system_score_gemma":0.00013105565,"threshold_uncertainty_score":0.99015963},"labels":[],"label_agreement":null},{"id":"W2417465401","doi":"10.1130/2006.2399(09)","title":"A fossil lycopsid forest succession in the classic Joggins section of Nova Scotia: Paleoecology of a disturbance-prone Pennsylvanian wetland","year":2006,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Botany and Plant Ecology Studies","field":"Agricultural and Biological Sciences","cited_by":58,"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":"Carboniferous; Pennsylvanian; Geology; Disturbance (geology); Paleontology; Peat; Paleoecology; Ecological succession; Wetland; Swamp; Nova scotia; Marsh; Horizon; Ecology; Structural basin; Geography; Archaeology; Oceanography","score_opus":0.01849993638445635,"score_gpt":0.20859394330068354,"score_spread":0.1900940069162272,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2417465401","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8112038,0.0011459514,0.000020237834,0.0013593183,0.00024498388,0.0008608739,0.00022318099,0.000036253878,0.18490542],"genre_scores_gemma":[0.9913763,0.00028821526,0.00015854892,0.00029664589,0.00020759991,0.000016873604,0.00008889188,0.0000024974288,0.0075644264],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.997985,0.00012637419,0.00074524595,0.00045879456,0.0002998625,0.00038468814],"domain_scores_gemma":[0.9978137,0.0009370151,0.00097056536,0.0001242328,0.00011332344,0.000041171406],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033370394,0.00036002102,0.0010406676,0.000017080933,0.00015566761,0.000007361497,0.00046032155,0.00078382733,0.00028443366],"category_scores_gemma":[0.00003067647,0.00013272016,0.0005134073,0.00009191709,0.0019680124,0.00002729194,0.00017651203,0.00060526974,0.000004509754],"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":[0.00071785215,0.00086096977,0.8911756,0.00044404765,0.00058516,0.000053814336,0.0012581673,0.000050441184,0.016564094,0.0033861718,0.034357198,0.05054646],"study_design_scores_gemma":[0.00044685838,0.0020711964,0.94448876,0.00016995225,0.00012444778,0.000024453566,0.0006445144,0.000021915897,0.0000860276,0.0050964653,0.046452258,0.00037315325],"about_ca_topic_score_codex":0.00137032,"about_ca_topic_score_gemma":0.018606516,"teacher_disagreement_score":0.18017252,"about_ca_system_score_codex":0.000034248653,"about_ca_system_score_gemma":0.000021881644,"threshold_uncertainty_score":0.9993014},"labels":[],"label_agreement":null},{"id":"W2418500297","doi":"10.1130/2010.1206(30)","title":"S and Z buckle folds as shear-sense indicators in the ductile realm: Field examples from the Grenville Province of Ontario and the Appalachians of South Carolina","year":2010,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Research Council Canada","keywords":"Geology; Shear zone; Overprinting; Schist; Sinistral and dextral; Shear (geology); Orogeny; Anticline; Thrust; Buckle; Thrust fault; Fold (higher-order function); Metamorphic rock; Paleontology; Structural basin; Tectonics","score_opus":0.009185544962294907,"score_gpt":0.17221463394898295,"score_spread":0.16302908898668805,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2418500297","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.86635816,0.0011063444,0.000009866364,0.0026355763,0.00002731184,0.000430673,0.00013532912,0.000008416104,0.12928835],"genre_scores_gemma":[0.9920485,0.00044202138,0.00077776634,0.0017674617,0.00005616444,0.0000039561455,0.00004581929,0.0000033761926,0.004854915],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99842584,0.00011672944,0.00047143173,0.00038931804,0.00035392522,0.00024274226],"domain_scores_gemma":[0.99726456,0.0017830682,0.00048175605,0.00036182115,0.00003804488,0.00007071813],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00044476733,0.00026064765,0.00072179805,0.000023283406,0.0001575454,0.000012821345,0.00042507655,0.0003918262,0.0024294434],"category_scores_gemma":[0.00010269174,0.000107016094,0.000325288,0.000061410465,0.00407723,0.000012180455,0.0001371997,0.00089293066,0.0000031631998],"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":[0.0012282713,0.00013394695,0.80956566,0.00016446975,0.0010362399,0.000031895903,0.05096012,0.00006745934,0.00018776512,0.009654363,0.001045963,0.12592386],"study_design_scores_gemma":[0.0018005184,0.0018440788,0.51552063,0.00012351136,0.0009317719,0.00004328948,0.0076713683,0.00023359373,0.00031067175,0.33773503,0.1329106,0.00087490404],"about_ca_topic_score_codex":0.1757554,"about_ca_topic_score_gemma":0.029498203,"teacher_disagreement_score":0.32808068,"about_ca_system_score_codex":0.0000032482594,"about_ca_system_score_gemma":0.000090819434,"threshold_uncertainty_score":0.9986331},"labels":[],"label_agreement":null},{"id":"W2436107576","doi":"10.1130/2014.0038(02)","title":"Applied geomorphology along the North Shore slopes of Burrard Inlet in North and West Vancouver","year":2014,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological formations and processes","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":"Simon Fraser University","funders":"","keywords":"Bedrock; Geology; Deglaciation; Shore; Geomorphology; Natural (archaeology); Glacial period; TRIPS architecture; Earth science; Archaeology; Oceanography; Paleontology; Geography","score_opus":0.013690360585503443,"score_gpt":0.1836848260703745,"score_spread":0.16999446548487107,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2436107576","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.38723928,0.0018224799,0.0011565014,0.0005900075,0.0002220115,0.0011011923,0.00054656144,0.000077268865,0.60724473],"genre_scores_gemma":[0.99043643,0.0006965021,0.0018180053,0.0014599266,0.000058594047,0.0000055130727,0.00024506854,0.0000058712,0.005274063],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983879,0.00004132461,0.00059844373,0.00036750498,0.00026744656,0.0003373847],"domain_scores_gemma":[0.9984991,0.00060679927,0.00047620866,0.0002465007,0.000081590195,0.00008979189],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00018562234,0.00031578983,0.0007603827,0.00003978769,0.0001280075,0.000012095844,0.00041011814,0.00034781237,0.0024247307],"category_scores_gemma":[0.00003119783,0.0001831962,0.0001905896,0.00006584755,0.0021793793,0.0000256111,0.000107132895,0.00053470506,0.000030824332],"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":[0.00014930153,0.000025898004,0.6437116,0.0003393213,0.00017245853,0.000010054316,0.0020555868,0.0022799645,0.0000020344542,0.0021673401,0.0048888675,0.34419754],"study_design_scores_gemma":[0.0004679527,0.0008547407,0.6578164,0.000046174897,0.00008884647,0.000013341344,0.00077744597,0.0004945396,0.000004109364,0.006856185,0.33200675,0.00057349424],"about_ca_topic_score_codex":0.0011211059,"about_ca_topic_score_gemma":0.012114012,"teacher_disagreement_score":0.60319716,"about_ca_system_score_codex":0.000003359561,"about_ca_system_score_gemma":0.00004141383,"threshold_uncertainty_score":0.9984872},"labels":[],"label_agreement":null},{"id":"W2463571132","doi":"10.1130/0-8137-2347-7.19","title":"Detrital zircon geochronology of the Roberts Mountains allochthon, Nevada","year":2000,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":46,"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":"Zircon; Geology; Allochthon; Provenance; Geochronology; Devonian; Ordovician; Paleozoic; Paleontology; Basement; Paleocurrent; Laurentia; Geochemistry; Conglomerate; Sedimentary depositional environment; Late Devonian extinction; Carboniferous; Nappe; Archaeology; Sedimentary rock; Structural basin; Tectonics; Geography","score_opus":0.010578689328678085,"score_gpt":0.17623395158422686,"score_spread":0.16565526225554877,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2463571132","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0285154,0.0017444154,0.00014051181,0.0010793676,0.00012255898,0.00037397334,0.000278097,0.000066321874,0.9676794],"genre_scores_gemma":[0.8448651,0.0012233972,0.005965495,0.0045332056,0.0002807148,0.0000050873973,0.0003513002,0.00001822339,0.1427575],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9974236,0.00007662404,0.000767846,0.00064218196,0.0005353727,0.0005543799],"domain_scores_gemma":[0.99817353,0.0003914003,0.0006272464,0.0005164732,0.00012202389,0.00016932475],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00015049677,0.00047843065,0.0011218555,0.00003691621,0.00016953178,0.0000112350945,0.0008832249,0.0007791322,0.03586967],"category_scores_gemma":[0.00004314697,0.00027743872,0.0015186981,0.000088030814,0.0031581712,0.000026975678,0.00016922598,0.0007712924,0.00013153194],"study_design_candidate":"design_other","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":[0.0006965223,0.0004123363,0.080787495,0.0004883908,0.003735926,0.0000803447,0.0009722502,0.0055754445,0.004222106,0.016298447,0.02074487,0.8659859],"study_design_scores_gemma":[0.00090891344,0.0018758114,0.037290215,0.0001690964,0.00085403805,0.00006978607,0.0002754984,0.0014102539,0.002149941,0.4674663,0.48589653,0.0016336313],"about_ca_topic_score_codex":0.0035079631,"about_ca_topic_score_gemma":0.0003068168,"teacher_disagreement_score":0.8643522,"about_ca_system_score_codex":0.000011400546,"about_ca_system_score_gemma":0.000072816416,"threshold_uncertainty_score":0.99996775},"labels":[],"label_agreement":null},{"id":"W2468729946","doi":"10.1130/0-8137-2347-7.43","title":"Detrital zircon geochronology of the Shoo Fly Complex, northern Sierra Terrane, northeastern California","year":2000,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":30,"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":"Zircon; Geology; Allochthon; Geochronology; Provenance; Basement; Terrane; Volcanic arc; Geochemistry; Paleozoic; Craton; Foreland basin; Paleontology; Archean; Baddeleyite; Archaeology; Subduction; Nappe; Tectonics; Geography","score_opus":0.0178613308893817,"score_gpt":0.18447992867261248,"score_spread":0.1666185977832308,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2468729946","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.14038153,0.0010825114,0.0002212308,0.0013511145,0.0001308746,0.00059253204,0.0015210342,0.00010266618,0.8546165],"genre_scores_gemma":[0.9700489,0.00023058425,0.0018788655,0.0021524164,0.00018744644,0.000003592247,0.0005236407,0.000015173715,0.024959357],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9970226,0.00009077199,0.0009312221,0.0007116233,0.0006078454,0.0006359372],"domain_scores_gemma":[0.99804306,0.0003145588,0.00071682286,0.00056993746,0.00014219258,0.00021340637],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00014478198,0.00056939194,0.0013219368,0.000043397118,0.0002094243,0.000013818198,0.0010187245,0.0007118718,0.03609736],"category_scores_gemma":[0.000029495915,0.000332902,0.0016424626,0.00009056173,0.0035481502,0.000022965765,0.00017989565,0.0008290977,0.00036752954],"study_design_candidate":"design_other","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":[0.00058282184,0.00028210814,0.31412038,0.00035228,0.0021649317,0.000048214766,0.0007677119,0.002846502,0.0025274225,0.00064820383,0.002716889,0.6729425],"study_design_scores_gemma":[0.0021069609,0.003463249,0.20200987,0.00031816764,0.0015821554,0.00016323256,0.0006377844,0.005915253,0.00097193004,0.22558486,0.5539299,0.0033165806],"about_ca_topic_score_codex":0.004039268,"about_ca_topic_score_gemma":0.0019786886,"teacher_disagreement_score":0.8296674,"about_ca_system_score_codex":0.000012097782,"about_ca_system_score_gemma":0.000072640774,"threshold_uncertainty_score":0.9999123},"labels":[],"label_agreement":null},{"id":"W2470734866","doi":"10.1130/0-8137-2343-4.61","title":"Reconnaissance geology and U-Pb geochronology of the west flank of the Coast Mountains between Bella Coola and Prince Rupert, coastal British Columbia","year":2000,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","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":"National Science Foundation","keywords":"Terrane; Geology; Zircon; Gondwana; Cretaceous; Paleontology; Assemblage (archaeology); Metamorphic rock; Shear zone; Continental margin; Geochemistry; Geomorphology; Tectonics","score_opus":0.010595652556294416,"score_gpt":0.17421912482160481,"score_spread":0.1636234722653104,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2470734866","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9021947,0.001875008,0.000014956732,0.000701465,0.000056361307,0.00041059908,0.00087755633,0.000022769798,0.09384663],"genre_scores_gemma":[0.97324085,0.0013001941,0.0004231191,0.000749931,0.00006575753,0.0000024710193,0.00007133292,0.0000064560595,0.024139894],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99780715,0.00013175256,0.0007145596,0.0006030081,0.00031184865,0.00043171257],"domain_scores_gemma":[0.9981305,0.00054491876,0.00069991546,0.00037645563,0.00011327143,0.00013493723],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00020013006,0.00030172634,0.00117099,0.000013531387,0.00028484722,0.000022909835,0.00063236064,0.00061279867,0.005516903],"category_scores_gemma":[0.000058709655,0.00021951951,0.0005091675,0.00006844326,0.009463588,0.000023147852,0.00039478374,0.00068691117,0.0000055568994],"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":[0.000038528688,0.00002583363,0.9067838,0.000110486355,0.00031732436,0.0000042792003,0.00014535047,0.000038363298,0.00010551423,0.00013993343,0.00094655214,0.09134404],"study_design_scores_gemma":[0.0004029567,0.00053526374,0.9336616,0.00012078979,0.0002500674,0.00007404445,0.00012680364,0.00014053835,0.00005832287,0.03442891,0.029826807,0.00037389967],"about_ca_topic_score_codex":0.05334395,"about_ca_topic_score_gemma":0.042056933,"teacher_disagreement_score":0.09097014,"about_ca_system_score_codex":0.000004669311,"about_ca_system_score_gemma":0.00006193196,"threshold_uncertainty_score":0.9953922},"labels":[],"label_agreement":null},{"id":"W2471977683","doi":"10.1130/2011.1207(14)","title":"Heterogeneous strain and polymetamorphism in high-grade terranes: Insight into crustal processes from the Athabasca Granulite Terrane, western Canada, and the Limpopo Complex, southern Africa","year":2011,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological Modeling and 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":"Geological Society of America; Russian Foundation for Basic Research; National Science Foundation","keywords":"Terrane; Granulite; Geology; Metamorphism; Tectonics; Shear zone; Geochemistry; Earth science; Metamorphic rock; Orogeny; Seismology; Paleontology; Facies","score_opus":0.028125562555836092,"score_gpt":0.18488384285523474,"score_spread":0.15675828029939864,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2471977683","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.84165245,0.064566046,0.0011953047,0.012518305,0.00030755348,0.0026676443,0.006619029,0.00026131506,0.070212334],"genre_scores_gemma":[0.98927796,0.0009800737,0.00054679444,0.0025769966,0.00010608437,0.0000072049147,0.00025971272,0.000012657287,0.0062325327],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9975425,0.00018825564,0.0006339709,0.0007165745,0.00045621645,0.00046245553],"domain_scores_gemma":[0.9981746,0.0008066965,0.00042978054,0.0003543215,0.000056689056,0.00017790838],"candidate_categories":["metaepi_narrow","sts"],"consensus_categories":[],"category_scores_codex":[0.0002639903,0.00053160044,0.001049569,0.000030887142,0.00033487685,0.000060822644,0.0005871411,0.00035162774,0.0007915074],"category_scores_gemma":[0.000036055106,0.0002635452,0.00025969697,0.000058273017,0.0028872096,0.000029630924,0.00014453009,0.00063505076,0.000007889018],"study_design_candidate":"design_other","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":[0.002079034,0.00025059847,0.18250567,0.00093137054,0.00432565,0.00042244614,0.154734,0.002039099,0.00008298647,0.0009010444,0.0016777138,0.6500504],"study_design_scores_gemma":[0.011032675,0.0037187843,0.34075865,0.0011608774,0.0041456814,0.00030841515,0.013557986,0.01899859,0.000027260012,0.2708975,0.32828054,0.007113033],"about_ca_topic_score_codex":0.7928163,"about_ca_topic_score_gemma":0.5985803,"teacher_disagreement_score":0.64293736,"about_ca_system_score_codex":0.000008809756,"about_ca_system_score_gemma":0.00011511762,"threshold_uncertainty_score":0.9999817},"labels":[],"label_agreement":null},{"id":"W2476982974","doi":"10.1130/2009.2461(21)","title":"The Integrated Ocean Drilling Program “School of Rock”: Lessons learned from an ocean-going research expedition for earth and ocean science educators","year":2009,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Reservoir Engineering and Simulation Methods","field":"Engineering","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":"Drilling; Ocean science; Research program; Earth science; Oceanography; Engineering; Geology; Mechanical engineering","score_opus":0.08069851110005992,"score_gpt":0.36321696001559256,"score_spread":0.2825184489155326,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2476982974","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7258966,0.0060192733,0.1372408,0.001728576,0.001396135,0.0076400484,0.00047891372,0.0028802434,0.116719425],"genre_scores_gemma":[0.79301274,0.0020905552,0.18138584,0.000097700235,0.0006881478,0.00003104387,0.00019440362,0.00015606589,0.022343472],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9976932,0.00007839182,0.00055268686,0.00052511145,0.00059263955,0.00055796903],"domain_scores_gemma":[0.99763316,0.0010345681,0.00018595504,0.00044489306,0.00044244432,0.00025897732],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0013581278,0.0003420006,0.00057309575,0.000120357545,0.0004647981,0.000104407,0.00050097896,0.0003772307,0.000024252398],"category_scores_gemma":[0.0003587573,0.00025910843,0.00027033934,0.00013892041,0.0011771383,0.00009074536,0.00010522482,0.0009547861,0.000001622431],"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":[0.0002042451,0.00013279518,0.00020657484,0.00043363002,0.000445316,0.0000026939001,0.003932912,0.3571582,0.0045865183,0.0047021504,0.0050996114,0.62309533],"study_design_scores_gemma":[0.0007711342,0.0015765424,0.000569387,0.00051303406,0.00009042474,0.0000027819224,0.0031129722,0.8017001,0.002564321,0.02989313,0.1583205,0.0008856833],"about_ca_topic_score_codex":0.000028063285,"about_ca_topic_score_gemma":6.902278e-7,"teacher_disagreement_score":0.62220967,"about_ca_system_score_codex":0.0000806012,"about_ca_system_score_gemma":0.00014521448,"threshold_uncertainty_score":0.9999861},"labels":[],"label_agreement":null},{"id":"W2477735327","doi":"10.1130/dnag-gna-o1.255","title":"Movement and storage of sediment in rivers of the United States and Canada","year":2015,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Soil erosion and sediment transport","field":"Agricultural and Biological Sciences","cited_by":354,"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":"Hydrology (agriculture); Surface runoff; Environmental science; Wetland; Hydrosphere; Precipitation; Sediment; Biota; Snow; Geology; Geography; Ecology; Geomorphology; Meteorology","score_opus":0.01967538737194274,"score_gpt":0.18792793525680196,"score_spread":0.16825254788485922,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2477735327","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98647696,0.00028975026,0.0000010534837,0.0006814297,0.00003943262,0.00029167644,0.00016781258,0.000007351769,0.012044563],"genre_scores_gemma":[0.9803275,0.0011479828,0.0001544649,0.0026130192,0.000021425207,0.0000062322893,0.0001086864,0.0000023172,0.015618406],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99894816,0.000025018204,0.00031633646,0.00019952573,0.00037286922,0.00013808183],"domain_scores_gemma":[0.99939954,0.00011597701,0.00027796577,0.00005565064,0.000074764306,0.000076122626],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013641817,0.00016188553,0.00039147475,0.000006406727,0.00003656893,0.0000023381297,0.00016156568,0.00014025798,0.00012219817],"category_scores_gemma":[0.000004669979,0.000057792946,0.00010461649,0.000030928797,0.0007419941,0.000006753333,0.00012527526,0.0001583428,7.180865e-8],"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":[0.001560727,0.0013313715,0.39152503,0.001623195,0.0022162404,0.000061518236,0.0148916645,0.0015628741,0.095433325,0.02947491,0.11521231,0.34510684],"study_design_scores_gemma":[0.0024803912,0.003631867,0.4144227,0.0007401987,0.0002872822,0.0000036193212,0.011878417,0.0007530658,0.0031807255,0.015804015,0.5454256,0.001392116],"about_ca_topic_score_codex":0.28672045,"about_ca_topic_score_gemma":0.022087334,"teacher_disagreement_score":0.4302133,"about_ca_system_score_codex":0.000036996684,"about_ca_system_score_gemma":0.000036864745,"threshold_uncertainty_score":0.99575704},"labels":[],"label_agreement":null},{"id":"W2478314607","doi":"10.1130/dnag-gna-p1.9","title":"Placer Uranium, Gold","year":2015,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Radioactive element chemistry and processing","field":"Chemistry","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":"Placer mining; Mineral; Section (typography); Uranium; Geology; Uranium ore; Mineral resource classification; Mineral deposit; Volume (thermodynamics); Placer deposit; Mining engineering; Mineralogy; Geochemistry; Business; Metallurgy; Materials science; Physics","score_opus":0.03714905390601861,"score_gpt":0.2536413368487474,"score_spread":0.2164922829427288,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2478314607","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00026862705,0.0011550367,0.00014840302,0.00013621846,0.000042580657,0.000073958916,0.00009371087,0.00014939386,0.9979321],"genre_scores_gemma":[0.01208118,0.00016479264,0.002753429,0.00054731744,0.00055808673,0.000015491629,0.00014440222,0.000062065024,0.9836732],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9978717,0.000008739288,0.0005215025,0.0006241029,0.0005488978,0.00042504008],"domain_scores_gemma":[0.99831724,0.00015913128,0.0006713167,0.0004362928,0.00020127605,0.00021476563],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00014184004,0.000537119,0.0008357258,0.000011910917,0.000091894275,0.000022050397,0.00046117493,0.0009502412,0.008480857],"category_scores_gemma":[0.000027704495,0.0004672557,0.00069935736,0.000015502927,0.0011427926,0.00003260023,0.00022399366,0.0010029054,0.000054807937],"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":[0.000734284,0.00026267924,0.00020398591,0.0035172012,0.0032647,0.000083087194,0.0020830287,0.000060118316,0.091689065,0.0093077775,0.53797716,0.3508169],"study_design_scores_gemma":[0.0004900351,0.000075025295,0.0000014513196,0.00018678834,0.00015173893,0.000017274595,0.00027260117,0.00005255149,0.009972803,0.010037409,0.97811604,0.0006262836],"about_ca_topic_score_codex":0.00001303971,"about_ca_topic_score_gemma":1.1418467e-7,"teacher_disagreement_score":0.44013888,"about_ca_system_score_codex":0.00014517107,"about_ca_system_score_gemma":0.00012855329,"threshold_uncertainty_score":0.9997779},"labels":[],"label_agreement":null},{"id":"W2480364652","doi":"10.1130/2011.0024(02)","title":"Classic Precambrian geology of northeast Minnesota","year":2011,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geology and Paleoclimatology Research","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":"Precambrian; Geology; Archaeology; Earth science; Mining engineering; Geochemistry; Geography","score_opus":0.03436516701625796,"score_gpt":0.2224211330455073,"score_spread":0.18805596602924934,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2480364652","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.012495145,0.0012102869,0.000077374294,0.00030382889,0.00018339124,0.000359936,0.00011414916,0.000049239883,0.98520666],"genre_scores_gemma":[0.6974073,0.0011648992,0.0035248448,0.00079488894,0.00014645547,0.0000058509754,0.00032945353,0.000018163795,0.29660812],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9974684,0.00014348021,0.00073513587,0.0006381054,0.00033498023,0.00067987345],"domain_scores_gemma":[0.997823,0.0005533331,0.00070866646,0.00052057573,0.00018709984,0.00020731948],"candidate_categories":["metaepi_narrow","sts","research_integrity","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003326397,0.0004383312,0.001268727,0.0000841773,0.00015013404,0.000003960205,0.0007263239,0.0013442071,0.015940372],"category_scores_gemma":[0.00003643444,0.00034353978,0.0007250257,0.000042147178,0.0063669,0.000031827778,0.0001298588,0.0009786678,0.0004557305],"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":[0.00021968533,0.000034602406,0.9583763,0.00016358323,0.0004151941,0.00002794816,0.0003617497,0.000008816803,0.000005067647,0.0065976772,0.0017667301,0.032022648],"study_design_scores_gemma":[0.0013036067,0.004729509,0.6086482,0.00018540653,0.00039739072,0.00034128304,0.00033867316,0.00043608234,0.00006373994,0.089181155,0.2928423,0.0015326953],"about_ca_topic_score_codex":0.00061351556,"about_ca_topic_score_gemma":0.00036375463,"teacher_disagreement_score":0.6885985,"about_ca_system_score_codex":0.0000020661469,"about_ca_system_score_gemma":0.00014470055,"threshold_uncertainty_score":0.99995226},"labels":[],"label_agreement":null},{"id":"W2482483420","doi":"10.1130/dnag-gna-f1.447","title":"Upper Paleozoic Rocks","year":2015,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","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":"","keywords":"Paleozoic; Geology; Graben; Mesozoic; Paleontology; Structural basin","score_opus":0.02611533327066849,"score_gpt":0.22426791277342473,"score_spread":0.19815257950275625,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2482483420","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00006585451,0.0016783368,0.0070847957,0.00012879695,0.00010347976,0.00014927612,0.000022711063,0.00035898335,0.99040776],"genre_scores_gemma":[0.07498604,0.0015871635,0.003723901,0.0010177429,0.00043988295,0.000035884346,0.0001680628,0.00013792941,0.9179034],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9984556,0.000015430907,0.0004664633,0.0003098904,0.00044381243,0.00030882444],"domain_scores_gemma":[0.9990999,0.00004805206,0.00014410703,0.0003768531,0.00012371047,0.00020735287],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000105276435,0.00039295445,0.00078753266,0.00005176793,0.00005278353,0.000013866569,0.00030116652,0.00063572056,0.0013981805],"category_scores_gemma":[0.000010562559,0.00031765192,0.00088568655,0.000034145338,0.00043465695,0.00002353112,0.0001135991,0.0005840696,0.00021968271],"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":[0.00006134392,0.00012623904,0.00028707442,0.00087157014,0.006823211,0.00006208998,0.004494924,0.09406981,0.0011260496,0.010848058,0.70469135,0.17653824],"study_design_scores_gemma":[0.00023241059,0.00012436384,0.000008425598,0.000047381323,0.00015906824,0.000003342504,0.0001765045,0.014814191,0.00006435567,0.009371367,0.974444,0.000554611],"about_ca_topic_score_codex":0.000014146255,"about_ca_topic_score_gemma":0.0000017139116,"teacher_disagreement_score":0.2697526,"about_ca_system_score_codex":0.00006724474,"about_ca_system_score_gemma":0.000033665587,"threshold_uncertainty_score":0.9999276},"labels":[],"label_agreement":null},{"id":"W2487479034","doi":"10.1130/dnag-gna-k1.441","title":"Quaternary Geology of the Queen Elizabeth Islands","year":2015,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":"","keywords":"Quaternary; Quaternary science; Geology; Structural geology; Earth science; Paleontology","score_opus":0.036716969842477166,"score_gpt":0.2473130147220685,"score_spread":0.21059604487959135,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2487479034","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.011555222,0.0014064641,0.000047269295,0.0010733149,0.00026573514,0.0003385241,0.00011083041,0.000038638012,0.985164],"genre_scores_gemma":[0.566375,0.00061006896,0.0012504244,0.0014335208,0.0001499435,0.0000033909491,0.00017011356,0.000012725154,0.42999482],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.997803,0.00020462816,0.00055595016,0.00044886227,0.00047072791,0.0005168737],"domain_scores_gemma":[0.9980535,0.0005145303,0.00056946557,0.0005231924,0.00019857903,0.00014074333],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004748502,0.00033791794,0.00093700824,0.00004087442,0.0001463009,0.0000043127516,0.00093155314,0.0010420288,0.0049085743],"category_scores_gemma":[0.000052639196,0.00020326511,0.00060756406,0.000039711736,0.005078128,0.000019227045,0.00021453721,0.0010167017,0.00018781224],"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":[0.000105390114,0.000013951697,0.98368764,0.000074776864,0.00022161489,0.000012167274,0.00038223996,0.000067446475,0.0000025339893,0.001708052,0.010406557,0.0033176034],"study_design_scores_gemma":[0.0016449699,0.0033454185,0.25751558,0.00019813076,0.00035430092,0.00025220047,0.00064424804,0.0017407332,0.00006981692,0.23482701,0.49808255,0.0013250514],"about_ca_topic_score_codex":0.00076879683,"about_ca_topic_score_gemma":0.000076146025,"teacher_disagreement_score":0.7261721,"about_ca_system_score_codex":0.0000029986934,"about_ca_system_score_gemma":0.00019117519,"threshold_uncertainty_score":0.99762946},"labels":[],"label_agreement":null},{"id":"W2488651736","doi":"10.1130/petrologic.1962.241","title":"Lead-Isotope and Potassium-Argon Studies in the East Kootenay District of British Columbia","year":2015,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","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":"","keywords":"Precambrian; Intrusion; Geology; Geochemistry; Isotope; Stock (firearms); Paleontology; Archaeology; Geography","score_opus":0.0537358354798092,"score_gpt":0.24567607296356375,"score_spread":0.19194023748375455,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2488651736","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0060819006,0.008771155,0.0028126908,0.0030789918,0.00021596125,0.0009897221,0.00012552636,0.00014506308,0.977779],"genre_scores_gemma":[0.4409677,0.002098579,0.01440224,0.002052725,0.00021766673,0.00008062177,0.000037781934,0.000019150471,0.5401235],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99789566,0.00008230772,0.00057531265,0.0006156526,0.00046696325,0.0003640856],"domain_scores_gemma":[0.9982195,0.00029473694,0.00056936394,0.00052756054,0.00031234295,0.000076516946],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00060437125,0.0002601038,0.00088912644,0.000014318348,0.000107553824,0.000059065555,0.0010528611,0.00038172977,0.000029777002],"category_scores_gemma":[0.00013074717,0.0002443997,0.0003119015,0.00007081363,0.0023767445,0.00004300098,0.0009350358,0.0005797228,0.000002765802],"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":[0.00005332573,0.000425406,0.002891007,0.0019255182,0.0010723978,0.00040703997,0.013731115,0.00013378791,0.0003815863,0.015848093,0.46006012,0.5030706],"study_design_scores_gemma":[0.001424371,0.001550919,0.006801797,0.001005848,0.00015730159,0.0004044012,0.0069984635,0.0012264284,0.000031294356,0.19445302,0.7844548,0.0014913578],"about_ca_topic_score_codex":0.0010904631,"about_ca_topic_score_gemma":0.00010612204,"teacher_disagreement_score":0.5015792,"about_ca_system_score_codex":0.000035137862,"about_ca_system_score_gemma":0.00006807605,"threshold_uncertainty_score":0.9966331},"labels":[],"label_agreement":null},{"id":"W2491537477","doi":"10.1130/dnag-gna-p1.287","title":"Arsenide Vein Silver, Uranium","year":2015,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Mineral; Uranium; Uranium ore; Section (typography); Volume (thermodynamics); Vein; Arsenide; Government (linguistics); Geology; Mineralogy; Metallurgy; Computer science; Materials science; Medicine; Physics; Surgery; Gallium arsenide; Optoelectronics; Philosophy","score_opus":0.036418770567949156,"score_gpt":0.25247017316068227,"score_spread":0.21605140259273312,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2491537477","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00045730622,0.001313357,0.00014995477,0.00015256219,0.000056150493,0.00007856973,0.00009288311,0.00016422049,0.997535],"genre_scores_gemma":[0.019189142,0.00023936284,0.0037396909,0.000626553,0.00067498913,0.000016315487,0.0001972349,0.000074154275,0.97524256],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9976577,0.000010828673,0.00058806903,0.00067528273,0.00059547817,0.00047262324],"domain_scores_gemma":[0.9981356,0.00017247965,0.00075071736,0.00048518006,0.00022105209,0.00023491633],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00015611129,0.0005753253,0.00091182615,0.000013830387,0.00013712286,0.000023960554,0.00050151726,0.00094763003,0.006278352],"category_scores_gemma":[0.0000384921,0.000515186,0.00080321264,0.00001816687,0.0012557743,0.0000373348,0.00023739164,0.001060054,0.000052567484],"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":[0.0007568502,0.00038296045,0.00023499988,0.003758339,0.0036675816,0.00014887778,0.0022045702,0.00010501741,0.23354203,0.009144332,0.3393669,0.40668753],"study_design_scores_gemma":[0.0005105163,0.000091472255,0.0000018461154,0.0001990648,0.00016684657,0.000020468304,0.00026916602,0.00007563859,0.021590043,0.014631666,0.96175116,0.00069208024],"about_ca_topic_score_codex":0.000017619921,"about_ca_topic_score_gemma":1.5991249e-7,"teacher_disagreement_score":0.6223843,"about_ca_system_score_codex":0.00015339244,"about_ca_system_score_gemma":0.00015596386,"threshold_uncertainty_score":0.99973},"labels":[],"label_agreement":null},{"id":"W2492808166","doi":"10.1130/dnag-gna-k1.699","title":"The Influence of the Quaternary Geology of Canada on Man’S Environment","year":2015,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Landslides and related hazards","field":"Environmental Science","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":"","keywords":"Quaternary; Geology; Quaternary science; Earth science; Physical geography; Paleontology; Geography","score_opus":0.009351486821088408,"score_gpt":0.1834786932228541,"score_spread":0.17412720640176568,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2492808166","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.15434481,0.00035832115,0.0000157225,0.001909415,0.0001757456,0.0005965785,0.000054121083,0.000014375877,0.8425309],"genre_scores_gemma":[0.7011047,0.0006897494,0.0002496171,0.0014236094,0.00003177173,0.000011925365,0.000004391736,0.00002359359,0.29646066],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99814194,0.000051603736,0.00047889614,0.00029707287,0.0007336966,0.00029680735],"domain_scores_gemma":[0.99846494,0.00017821026,0.00071311434,0.0005395706,0.000017988279,0.00008619324],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00021527335,0.00024921895,0.00044690073,0.0000044700914,0.00014075708,0.0000021778415,0.00074286666,0.0003247065,0.0006789878],"category_scores_gemma":[0.000016412716,0.000116598,0.00032395095,0.000014504653,0.0034928203,0.000008423861,0.00075877184,0.00047171096,0.000016937942],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016493758,0.0006236061,0.06055522,0.0004072562,0.0033841075,0.00009737968,0.0057277614,0.29042056,0.0062042917,0.037811108,0.4491813,0.14393803],"study_design_scores_gemma":[0.0004263629,0.00091564836,0.024701484,0.00009778387,0.00011175181,0.000013667001,0.00020540046,0.00029450632,0.00032235697,0.020578597,0.95190144,0.0004309884],"about_ca_topic_score_codex":0.045140024,"about_ca_topic_score_gemma":0.001169755,"teacher_disagreement_score":0.5467599,"about_ca_system_score_codex":0.00019970337,"about_ca_system_score_gemma":0.00009315843,"threshold_uncertainty_score":0.9992191},"labels":[],"label_agreement":null},{"id":"W2492861622","doi":"10.1130/dnag-gna-i1.167","title":"The Geology of the Southeastern Margin of Canada","year":2015,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":92,"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; Paleontology; Continental margin; Quaternary; Cenozoic; Tectonics; Sedimentary rock; Basement; Bathymetry; Phanerozoic; Passive margin; Rift; Oceanography; Structural basin; Archaeology; Geography","score_opus":0.028020284725918873,"score_gpt":0.18365521742255336,"score_spread":0.15563493269663448,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2492861622","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0069829957,0.0031553917,0.000075810545,0.0034946688,0.00044709985,0.00048972166,0.00021580972,0.000016400216,0.9851221],"genre_scores_gemma":[0.80280334,0.00054832804,0.00048969855,0.0010933055,0.00014597506,0.000003558658,0.00004589323,0.000008118112,0.19486177],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9983749,0.00006965763,0.0005075379,0.00022962951,0.0005014179,0.00031686138],"domain_scores_gemma":[0.99830574,0.00039304682,0.00072811445,0.00030137663,0.00019530689,0.000076405675],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029049424,0.00021860354,0.0005680775,0.000005883971,0.0002154761,0.0000039753927,0.00055267464,0.00023791597,0.00076173485],"category_scores_gemma":[0.00006123776,0.00009940253,0.00034151817,0.000027236967,0.0022666857,0.000008901591,0.00015687938,0.00031410134,0.000007734758],"study_design_candidate":"not_applicable","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":[0.0010122183,0.00009053917,0.19717847,0.0004897548,0.0024031186,0.000015151784,0.0041169217,0.007935036,0.000044236738,0.041098587,0.20560686,0.5400091],"study_design_scores_gemma":[0.0003502779,0.0009038877,0.0503642,0.000055088425,0.000101308084,0.0000067711544,0.0026823285,0.0009266623,0.000017250262,0.0645301,0.8796749,0.00038723214],"about_ca_topic_score_codex":0.13492097,"about_ca_topic_score_gemma":0.08224489,"teacher_disagreement_score":0.79582036,"about_ca_system_score_codex":0.0000074327754,"about_ca_system_score_gemma":0.00020866227,"threshold_uncertainty_score":0.93450177},"labels":[],"label_agreement":null},{"id":"W2496130316","doi":"10.1130/dnag-gna-f1.891","title":"Caledonides of East Greenland","year":2015,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological Studies and Exploration","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":"","keywords":"Paleozoic; Geology; Graben; Mesozoic; Paleontology; Earth science; Structural basin","score_opus":0.05578800842470636,"score_gpt":0.2136333671087245,"score_spread":0.15784535868401814,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2496130316","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0019257305,0.0022554637,0.0003031953,0.0003603489,0.000116620344,0.00025271397,0.00018953269,0.00004691831,0.99454945],"genre_scores_gemma":[0.59267545,0.0023611935,0.014115497,0.0016168441,0.0006201428,0.0000061879905,0.00068130693,0.000023369124,0.3879],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.998399,0.000029455538,0.00048729315,0.000347279,0.00044054614,0.00029638864],"domain_scores_gemma":[0.99882287,0.00014209394,0.0004919882,0.00020092037,0.00019512312,0.00014698268],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00020916875,0.00029003076,0.00079902494,0.000018828161,0.00009739536,0.0000070375536,0.00026759965,0.00039340116,0.0037024098],"category_scores_gemma":[0.00003299817,0.00019180297,0.00043975524,0.000025689622,0.0014512388,0.000025175672,0.00008119566,0.00030080817,0.0001178054],"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":[0.00041681464,0.00007808529,0.051356632,0.00035263156,0.00089946395,0.000025829471,0.0018089435,0.0015584596,0.000028207836,0.007127947,0.08323452,0.85311246],"study_design_scores_gemma":[0.0006064939,0.0029163086,0.021083169,0.00011555921,0.00017716143,0.000011454189,0.0011243524,0.0010991051,0.000011379543,0.09688016,0.8751839,0.00079099013],"about_ca_topic_score_codex":0.0010559306,"about_ca_topic_score_gemma":0.000073565665,"teacher_disagreement_score":0.85232145,"about_ca_system_score_codex":0.0000060077427,"about_ca_system_score_gemma":0.000038247195,"threshold_uncertainty_score":0.99720836},"labels":[],"label_agreement":null},{"id":"W2498356914","doi":"10.1130/2007.2425(22)","title":"Horizontal-to-vertical ground motion relations at short distances for four hard-rock sites in eastern Canada and implications for seismic hazard assessment","year":2007,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Seismic Performance and Analysis","field":"Engineering","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":"","keywords":"Magnitude (astronomy); Seismometer; Seismology; Ground motion; Geology; Seismic hazard; Hazard analysis; Range (aeronautics); Horizontal and vertical; Hazard; Geodesy; Geography; Engineering; Physics","score_opus":0.03444186142933397,"score_gpt":0.2555184090970875,"score_spread":0.22107654766775353,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2498356914","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.14045969,0.0004428729,0.8233748,0.0016980866,0.0001396344,0.0017362237,0.0006689291,0.000152467,0.031327326],"genre_scores_gemma":[0.9611169,0.00017905004,0.015193821,0.0007924719,0.00013954309,0.0002524616,0.00032946555,0.000049282968,0.02194698],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9986535,0.0000050005683,0.00045714134,0.0003500913,0.00019597913,0.00033831503],"domain_scores_gemma":[0.9993252,0.00021425854,0.000063278196,0.00017535544,0.00009982632,0.00012207215],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00012449638,0.00027226302,0.0005146988,0.00004949093,0.00014648853,0.000015628111,0.00013187503,0.0002388206,0.00002066873],"category_scores_gemma":[0.00001200769,0.000254041,0.000280028,0.000037355097,0.00010928197,0.00003700601,0.00006242295,0.00020957527,0.0000016205433],"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":[0.00042457762,0.0002487874,0.12135651,0.0025055727,0.004871773,0.000012831783,0.0020560024,0.10702493,0.007235448,0.01684335,0.14290617,0.594514],"study_design_scores_gemma":[0.000936688,0.00060938025,0.076285325,0.0002137473,0.0006517717,0.000012557946,0.0005054305,0.57218474,0.00009437068,0.008965747,0.33806655,0.0014736752],"about_ca_topic_score_codex":0.0027181078,"about_ca_topic_score_gemma":0.01692978,"teacher_disagreement_score":0.82065725,"about_ca_system_score_codex":0.0005614724,"about_ca_system_score_gemma":0.00006907258,"threshold_uncertainty_score":0.9999912},"labels":[],"label_agreement":null},{"id":"W2503279152","doi":"10.1130/2014.2503(08)","title":"Euselachians from the freshwater deposits of the Hell Creek Formation of Montana","year":2014,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Evolution and Paleontology Studies","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":"Royal Tyrrell Museum; University of Alberta","funders":"University of Alberta","keywords":"Geology; Geochemistry","score_opus":0.019305577224334815,"score_gpt":0.1874735304524005,"score_spread":0.1681679532280657,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2503279152","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.028657898,0.0034168917,0.002103252,0.001397177,0.00028188483,0.0005864882,0.0008009488,0.00004034532,0.9627151],"genre_scores_gemma":[0.9380448,0.00066089496,0.0030334012,0.0030550696,0.00013185892,0.0000023575517,0.00012922859,0.000007181004,0.054935247],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99879426,0.00009815666,0.00044920115,0.00018868774,0.0002882894,0.00018142183],"domain_scores_gemma":[0.9984576,0.0004910787,0.0006380599,0.0002928623,0.00008425542,0.00003611279],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014656516,0.00018560981,0.00048420212,0.000008248778,0.00018827686,0.000005329181,0.00044695247,0.0002678116,0.00053406454],"category_scores_gemma":[0.000020835641,0.00009564345,0.00048018878,0.000018073653,0.0017667745,0.000016327025,0.00006094178,0.0003047669,0.000017778266],"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":[0.00016088423,0.000042213745,0.8413665,0.00023460008,0.001274004,0.0000023446148,0.008569058,0.00047860027,0.00013793186,0.0033112136,0.0668716,0.077551],"study_design_scores_gemma":[0.0005470958,0.0007376343,0.6835614,0.00020983185,0.00043002338,0.000009111517,0.0013482163,0.0018493829,0.00018166481,0.015800808,0.2948588,0.0004660562],"about_ca_topic_score_codex":0.004921169,"about_ca_topic_score_gemma":0.04009794,"teacher_disagreement_score":0.9093869,"about_ca_system_score_codex":0.0000032452654,"about_ca_system_score_gemma":0.000020153037,"threshold_uncertainty_score":0.97741777},"labels":[],"label_agreement":null},{"id":"W2504227489","doi":"10.1130/dnag-gna-k1.481","title":"Quaternary Environments in Canada as Documented by Paleobotanical Case Histories","year":2015,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geology and Paleoclimatology Research","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":"","keywords":"Quaternary; Geology; Quaternary science; Paleontology; Physical geography; Earth science; Archaeology; Geography","score_opus":0.023260112343143152,"score_gpt":0.22423642111901299,"score_spread":0.20097630877586983,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2504227489","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.089334756,0.006072628,0.000018796189,0.0011018537,0.00035123105,0.00056731846,0.00036132915,0.000034683304,0.9021574],"genre_scores_gemma":[0.7606574,0.00052674976,0.0003546142,0.0011741158,0.00004069768,0.0000052487107,0.0003574339,0.000010044594,0.23687367],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99761796,0.00014009794,0.00054306205,0.00056121184,0.00053564983,0.0006020257],"domain_scores_gemma":[0.99867344,0.00040262257,0.00028894652,0.00029789956,0.000030612104,0.00030646587],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00026134384,0.00037157282,0.0007930011,0.000026667316,0.00012026843,0.0000064552883,0.00039348705,0.00057282427,0.00889857],"category_scores_gemma":[0.000030829302,0.00030838078,0.0001897243,0.000023370794,0.0016229238,0.000030497733,0.00009490979,0.00097543193,0.0001680063],"study_design_candidate":"not_applicable","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":[0.00016900594,0.000021039368,0.96495366,0.000036540623,0.00017187149,0.003332897,0.0002299778,0.000057523408,0.0000026739851,0.00015226284,0.0254605,0.0054120435],"study_design_scores_gemma":[0.0012742344,0.0013063715,0.010148805,0.000057044086,0.00010139905,0.0022018165,0.0012396027,0.0007160196,0.000012444732,0.009710363,0.9720983,0.0011336188],"about_ca_topic_score_codex":0.6715599,"about_ca_topic_score_gemma":0.49552295,"teacher_disagreement_score":0.95480484,"about_ca_system_score_codex":0.000058326063,"about_ca_system_score_gemma":0.00054136815,"threshold_uncertainty_score":0.9999368},"labels":[],"label_agreement":null},{"id":"W2504951280","doi":"10.1130/dnag-csms-neo.445","title":"Heat flux in the Canadian Cordillera","year":2015,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","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":"Induced seismicity; Neotectonics; Geology; Geothermal gradient; Scale (ratio); Geodynamics; Seismology; Geography; Cartography; Geophysics; Fault (geology); Tectonics","score_opus":0.03153289714140321,"score_gpt":0.2030765660727162,"score_spread":0.171543668931313,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2504951280","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.002870576,0.0008513483,0.0000039460538,0.0024127155,0.000048380745,0.00022348392,0.00011620167,0.000023618051,0.99344975],"genre_scores_gemma":[0.8356155,0.00016121636,0.0012033043,0.013294528,0.00023124264,0.00000550062,0.0007587734,0.000008189168,0.14872171],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9979031,0.00006854625,0.00043784856,0.0004586379,0.0005831665,0.00054866506],"domain_scores_gemma":[0.9988534,0.00027396393,0.00009801495,0.0003247208,0.000117290045,0.00033260093],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00035576467,0.000345034,0.00072026474,0.000048399204,0.00017322863,0.000028580645,0.00069936644,0.00053094886,0.037390064],"category_scores_gemma":[0.00004467766,0.00018974769,0.00056734786,0.00007671964,0.0013133936,0.000018275881,0.000046730664,0.000841585,0.00040560684],"study_design_candidate":"not_applicable","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":[0.00027441184,0.00020953453,0.10341702,0.00023905038,0.0014654588,0.00052967435,0.0037489643,0.0031602562,0.000058069607,0.013860087,0.3926333,0.4804042],"study_design_scores_gemma":[0.00028686627,0.00060584355,0.014573474,0.000040292518,0.00013417439,0.000020057449,0.0004870574,0.002067386,0.000005777009,0.14412175,0.8369912,0.0006660972],"about_ca_topic_score_codex":0.23563343,"about_ca_topic_score_gemma":0.12791419,"teacher_disagreement_score":0.844728,"about_ca_system_score_codex":0.000022354701,"about_ca_system_score_gemma":0.00016281242,"threshold_uncertainty_score":0.9634899},"labels":[],"label_agreement":null},{"id":"W2505720066","doi":"10.1130/2015.1212(13)","title":"Climate and tectonics along the southern margin of the Puna Plateau, NW Argentina: Origin of the late Cenozoic Punaschotter conglomerates","year":2015,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Geological Society of America","keywords":"Geology; Facies; Diachronous; Plateau (mathematics); Paleontology; Tectonics; Cenozoic; Alluvial fan; Geomorphology; Structural basin","score_opus":0.03078944430698013,"score_gpt":0.23054890285388452,"score_spread":0.19975945854690438,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2505720066","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.82651305,0.004274063,0.0000041079365,0.0017546401,0.00029324414,0.0008889874,0.00053373,0.000028069953,0.1657101],"genre_scores_gemma":[0.9448365,0.0010190284,0.00022392924,0.00080775423,0.000049650225,0.000004964728,0.000046885154,0.000013926792,0.052997388],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99770105,0.000295743,0.00059587794,0.00036618218,0.0004826873,0.00055847474],"domain_scores_gemma":[0.9976918,0.00069031137,0.0007684304,0.00057330466,0.00018204203,0.00009409627],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00093454326,0.00035609846,0.0007776626,0.00002542051,0.0003728328,0.0000150945925,0.000944052,0.0005923062,0.0014900666],"category_scores_gemma":[0.000059561782,0.00015764209,0.0005187968,0.00007162434,0.006628312,0.000023613362,0.000321663,0.0011212141,0.00006324348],"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":[0.000113620044,0.000014722113,0.993891,0.00014419775,0.0003050696,0.0000034826173,0.0010899529,0.00012713116,0.000026621645,0.00094402494,0.00093420397,0.0024059447],"study_design_scores_gemma":[0.002266606,0.0011964154,0.79658896,0.0005918574,0.0008824678,0.00022831526,0.003463611,0.0022916317,0.00046208326,0.04487426,0.14574772,0.0014060615],"about_ca_topic_score_codex":0.00045264442,"about_ca_topic_score_gemma":0.00022777762,"teacher_disagreement_score":0.19730206,"about_ca_system_score_codex":0.0000029671792,"about_ca_system_score_gemma":0.00012324944,"threshold_uncertainty_score":0.9994227},"labels":[],"label_agreement":null},{"id":"W2506161443","doi":"10.1130/dnag-gna-k1.665","title":"Quaternary Resources in Canada","year":2015,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geology and Paleoclimatology Research","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":"","keywords":"Quaternary; Geology; Quaternary science; Earth science; Paleontology; Physical geography; Geography","score_opus":0.03691550605571088,"score_gpt":0.225220833860783,"score_spread":0.18830532780507214,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2506161443","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.04284218,0.002202078,0.000003250304,0.0005144451,0.000118250806,0.00018884853,0.00007783986,0.000020963465,0.9540321],"genre_scores_gemma":[0.734141,0.00041017265,0.0008704919,0.0016642568,0.00010056887,0.0000027634492,0.00018078493,0.000009583814,0.26262036],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9981059,0.000094231975,0.00042181913,0.00041748091,0.0004461455,0.00051444775],"domain_scores_gemma":[0.99883395,0.0004098583,0.00023806865,0.00025332303,0.00007160924,0.00019318747],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00029640077,0.00027508533,0.00071059284,0.000041240197,0.00007315805,0.0000053450044,0.0004882096,0.0004765576,0.0052431487],"category_scores_gemma":[0.000024867471,0.00021442017,0.00018397297,0.00002726366,0.0012042662,0.000016513504,0.000076830125,0.00088238606,0.00014780874],"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":[0.00006913722,0.0000039875035,0.982485,0.000035524128,0.00006288494,0.00012067358,0.00018571207,0.0001453308,2.1313794e-7,0.00016137079,0.008021404,0.008708766],"study_design_scores_gemma":[0.0008448638,0.0008703829,0.2670539,0.00013818734,0.000057008743,0.00012989626,0.0011957047,0.0023294396,0.000003949933,0.03912204,0.68722284,0.001031788],"about_ca_topic_score_codex":0.7258129,"about_ca_topic_score_gemma":0.72272104,"teacher_disagreement_score":0.7154311,"about_ca_system_score_codex":0.00001577991,"about_ca_system_score_gemma":0.00072282087,"threshold_uncertainty_score":0.9956662},"labels":[],"label_agreement":null},{"id":"W2506179173","doi":"10.1130/dnag-gna-f1.21","title":"Temporal and spatial divisions","year":2015,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Regional Economics and Spatial Analysis","field":"Economics, Econometrics and Finance","cited_by":28,"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":"Paleozoic; Geology; Graben; Mesozoic; Paleontology; Earth science; Physical geography; Geography; Structural basin","score_opus":0.057441889037756724,"score_gpt":0.22111979519083585,"score_spread":0.16367790615307914,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2506179173","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00060177967,0.0025012458,0.0067910594,0.0014536614,0.00010853492,0.00020148406,0.0003679907,0.000034743076,0.9879395],"genre_scores_gemma":[0.36803094,0.0027199658,0.006742659,0.0020642416,0.00046524295,0.000022353468,0.00022253074,0.00008260048,0.61964947],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.99830353,0.0000062898685,0.0007994338,0.0005798058,0.00006891952,0.0002420192],"domain_scores_gemma":[0.99847513,0.000069195215,0.0008968953,0.0003029755,0.000066557535,0.00018925723],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00024845367,0.00030503699,0.0011764537,0.00006678867,0.00009711048,0.000027359229,0.00024312781,0.00042670782,0.0010165877],"category_scores_gemma":[0.000023045013,0.000293788,0.0006993613,0.000016842283,0.0008286392,0.000026376862,0.00029502617,0.00032280944,0.00014540335],"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":[0.00003472411,0.000054386222,0.0034255537,0.000051767285,0.00081813906,0.0000057028524,0.00032526313,0.000048519298,0.00000229001,0.9152559,0.025026228,0.054951537],"study_design_scores_gemma":[0.00020606873,0.00019355786,0.00038332026,0.000013602401,0.000027511795,0.0000020162624,0.00002642789,0.0024175711,4.111269e-7,0.34711242,0.6493,0.00031713047],"about_ca_topic_score_codex":0.002586759,"about_ca_topic_score_gemma":0.000028339786,"teacher_disagreement_score":0.6242737,"about_ca_system_score_codex":0.00005987703,"about_ca_system_score_gemma":0.000031767417,"threshold_uncertainty_score":0.9999514},"labels":[],"label_agreement":null},{"id":"W2506413574","doi":"10.1130/dnag-gna-k1.391","title":"Quaternary Geology of the Atlantic Appalachian Region of Canada","year":2015,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":107,"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":"Quaternary; Geology; Quaternary science; Earth science; Paleontology; Physical geography; Archaeology; Geomorphology; Geography","score_opus":0.03328751422146555,"score_gpt":0.2163045036691621,"score_spread":0.18301698944769654,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2506413574","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.13181597,0.0014105416,0.000038203387,0.0016123813,0.000352726,0.0004713883,0.00007152197,0.000019912666,0.8642074],"genre_scores_gemma":[0.916026,0.00014930363,0.00028721007,0.0004242962,0.000042773412,0.0000010983944,0.00005789675,0.0000052367695,0.08300619],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9980369,0.0001822877,0.00055569835,0.00033658097,0.0004581588,0.0004303294],"domain_scores_gemma":[0.9980505,0.0004788318,0.0007244819,0.00044008752,0.00018019823,0.00012587414],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003146521,0.0002613542,0.00087820494,0.000029776274,0.00010924971,0.0000015625865,0.0007381497,0.0006083999,0.0011562667],"category_scores_gemma":[0.000054774264,0.00016432325,0.00037729132,0.000036491303,0.0039116526,0.000011283967,0.00013537955,0.0006841199,0.000011542084],"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":[0.000092833936,0.000008946709,0.98940516,0.00012255192,0.00015423336,0.000022500622,0.00015031068,0.00011903777,0.0000018330285,0.0011472575,0.007606184,0.0011691295],"study_design_scores_gemma":[0.0017303064,0.0031458063,0.67914677,0.0004133245,0.00043011634,0.00090134813,0.0010024795,0.0026311113,0.000087120505,0.10667665,0.2023864,0.0014485584],"about_ca_topic_score_codex":0.18749839,"about_ca_topic_score_gemma":0.09308926,"teacher_disagreement_score":0.78421,"about_ca_system_score_codex":0.000004857493,"about_ca_system_score_gemma":0.0006399948,"threshold_uncertainty_score":0.9997568},"labels":[],"label_agreement":null},{"id":"W2533711595","doi":"10.1130/2018.2535(19)","title":"Live science in the <i>Valley of the Last Dinosaurs</i> : A public window into the world of paleontology","year":2018,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Species Distribution and Climate Change","field":"Environmental Science","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":"","keywords":"Outreach; Social media; Timeline; Library science; History; Visual arts; Media studies; Archaeology; Art; Sociology; Political science; World Wide Web; Computer science","score_opus":0.028745873145318294,"score_gpt":0.23731951008970126,"score_spread":0.20857363694438297,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2533711595","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.080000065,0.00013687924,0.000015268717,0.0039860485,0.00011961358,0.0005725595,0.0000430445,0.000014747055,0.9151118],"genre_scores_gemma":[0.9741161,0.00018720179,0.00017222854,0.0043249745,0.000047566882,0.0000374033,0.0000080242135,0.000011348995,0.021095185],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99773663,0.00010839328,0.00049120846,0.0004192051,0.0008355873,0.0004089499],"domain_scores_gemma":[0.9980249,0.00042645424,0.000731436,0.0006842405,0.000072686904,0.000060276463],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0007709642,0.0002516801,0.00045994713,0.00002341866,0.0002751882,0.000017246886,0.0020440824,0.00019422184,0.015725909],"category_scores_gemma":[0.00012519941,0.00011772735,0.00046036078,0.00023559204,0.023117684,0.00003814815,0.0011129313,0.00047722104,0.00006551911],"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":[0.00036731697,0.0017953732,0.31184658,0.00036894256,0.0006195615,0.000017197823,0.14287406,0.000038080394,0.018126016,0.24668384,0.1751933,0.10206975],"study_design_scores_gemma":[0.00059216167,0.00071389286,0.3946947,0.00013055596,0.000103638515,0.000015513764,0.023960132,0.00003527479,0.00045286928,0.012842033,0.5659406,0.00051861565],"about_ca_topic_score_codex":0.0004268703,"about_ca_topic_score_gemma":0.0022701288,"teacher_disagreement_score":0.894116,"about_ca_system_score_codex":0.00018567836,"about_ca_system_score_gemma":0.0000561299,"threshold_uncertainty_score":0.9851738},"labels":[],"label_agreement":null},{"id":"W2773574057","doi":"10.1130/2018.2541(19)","title":"Detrital zircon U-Pb geochronological and Hf isotopic constraints on the geological evolution of North Yukon","year":2019,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","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":"Yukon University","funders":"","keywords":"Geology; Zircon; Terrane; Carboniferous; Paleozoic; Laurentia; Devonian; Paleontology; Precambrian; Conglomerate; Ordovician; North American Plate; Orogeny; Tectonics; Structural basin; Plate tectonics","score_opus":0.01466139068701259,"score_gpt":0.17697977304388338,"score_spread":0.1623183823568708,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2773574057","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.46250638,0.0011722952,0.00077448186,0.001440201,0.00012108013,0.0008586403,0.00037824202,0.00009998733,0.5326487],"genre_scores_gemma":[0.9849527,0.00036454995,0.0018389324,0.0012804518,0.00010800165,0.000003883665,0.0001483775,0.0000065170234,0.011296609],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9970255,0.00011062126,0.00079318596,0.00086803164,0.0006090555,0.00059362827],"domain_scores_gemma":[0.9971345,0.0013882685,0.000680944,0.00043888122,0.00015478852,0.00020263839],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00028836113,0.0005719897,0.0012745346,0.000055997956,0.00018847674,0.000018516377,0.0006010423,0.0007894167,0.015581176],"category_scores_gemma":[0.00016388836,0.00030985617,0.0008873408,0.00008588906,0.0064549707,0.000036988706,0.00021287007,0.0010791277,0.00020720117],"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":[0.00088731386,0.00047119102,0.36534646,0.0005196563,0.002132678,0.000087553606,0.00033925794,0.0010580801,0.0015534852,0.10023813,0.0039042176,0.523462],"study_design_scores_gemma":[0.0012820765,0.007708626,0.7464494,0.00021941988,0.00062228827,0.000073451934,0.00048202384,0.0022219245,0.00048304154,0.21454524,0.02410064,0.0018118684],"about_ca_topic_score_codex":0.00050881703,"about_ca_topic_score_gemma":0.00010669839,"teacher_disagreement_score":0.5224463,"about_ca_system_score_codex":0.00001987898,"about_ca_system_score_gemma":0.00007182549,"threshold_uncertainty_score":0.9999353},"labels":[],"label_agreement":null},{"id":"W2780390045","doi":"","title":"Review of the Proterozoic evolution of the Grenville Province, its Adirondack outlier, and the Mesoproterozoic inliers of the Appalachians","year":2010,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","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":"","keywords":"Laurentia; Geology; Proterozoic; Rodinia; Orogeny; Geochronology; Precambrian; Terrane; Amazonian; Crust; Paleontology; Geochemistry; Craton; Earth science; Tectonics; Amazon rainforest","score_opus":0.007576115353038164,"score_gpt":0.1710035614460745,"score_spread":0.16342744609303633,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2780390045","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.18557185,0.14401078,0.00021467984,0.030062582,0.00089192746,0.018345667,0.0016776401,0.00009354044,0.6191313],"genre_scores_gemma":[0.95205534,0.0052833874,0.0006623362,0.003817238,0.000096418815,0.000031173102,0.000020305064,0.000012213012,0.03802162],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99748796,0.00026889605,0.0008530897,0.00041703248,0.00066631957,0.00030668522],"domain_scores_gemma":[0.9970325,0.00030103658,0.0016547749,0.0007648452,0.00017379933,0.00007301759],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00061395345,0.00036198573,0.0010492835,0.000014844488,0.00027012642,0.000006449354,0.0013291512,0.00040360825,0.0012450026],"category_scores_gemma":[0.00022765239,0.00012349951,0.0014561958,0.0001316557,0.008199602,0.000017949395,0.00042487137,0.0010232377,0.000005185599],"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":[0.0020783055,0.0009968206,0.4358432,0.049665175,0.007672128,0.0000045302177,0.0060021626,0.0008913214,0.011060487,0.06448702,0.016907172,0.4043917],"study_design_scores_gemma":[0.0039362744,0.0021026183,0.3538314,0.012952344,0.0051570726,0.00006613799,0.0009250867,0.003151631,0.0048603523,0.26761043,0.34303984,0.0023667929],"about_ca_topic_score_codex":0.0011322261,"about_ca_topic_score_gemma":0.00021052173,"teacher_disagreement_score":0.7664835,"about_ca_system_score_codex":0.000008201957,"about_ca_system_score_gemma":0.00011441688,"threshold_uncertainty_score":0.999668},"labels":[],"label_agreement":null},{"id":"W2781538727","doi":"","title":"Response of synorogenic plutons in the middle crust of continental magmatic arcs to regional tectonic changes; an example from the Coast Mountains of British Columbia","year":2009,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":0,"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":"Pluton; Geology; Crust; Continental crust; Tectonics; Continental margin; Geochemistry; Seismology","score_opus":0.0395028534296072,"score_gpt":0.20039864659459802,"score_spread":0.1608957931649908,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2781538727","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9896091,0.0007071294,0.000014053793,0.000700851,0.0000145668055,0.0004657606,0.0010378031,0.000013525259,0.0074371784],"genre_scores_gemma":[0.9916437,0.00016848034,0.0010968472,0.002259101,0.000038436185,0.0000061375727,0.00028606423,0.0000049776067,0.00449624],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9975205,0.0002612227,0.00077596394,0.00046140756,0.000622183,0.00035873882],"domain_scores_gemma":[0.99711597,0.001508362,0.0006706853,0.00045220958,0.0001346236,0.00011812145],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00066073297,0.00024158527,0.0010393489,0.000026765514,0.00008954682,0.000018501089,0.0009060545,0.0003046853,0.0037056943],"category_scores_gemma":[0.00007177891,0.00018072365,0.0006349399,0.00013960314,0.0019993493,0.00001966631,0.00009933624,0.00042214405,0.000005643612],"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":[0.00996291,0.0035348828,0.34891126,0.00096460443,0.0050839684,0.00026488033,0.041135516,0.0029936566,0.025175394,0.0013841997,0.048720036,0.5118687],"study_design_scores_gemma":[0.0014762194,0.0052395016,0.9189841,0.00062979665,0.00060361455,0.000058243113,0.012421482,0.001085063,0.00018580985,0.0367674,0.021586541,0.0009622174],"about_ca_topic_score_codex":0.2637266,"about_ca_topic_score_gemma":0.119007036,"teacher_disagreement_score":0.5700729,"about_ca_system_score_codex":0.00000892735,"about_ca_system_score_gemma":0.00006278283,"threshold_uncertainty_score":0.9972051},"labels":[],"label_agreement":null},{"id":"W2782247731","doi":"","title":"Retention of metals in a floodplain environment, Ottawa River, NW Ohio","year":2012,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Heavy metals in environment","field":"Environmental Science","cited_by":0,"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":"Floodplain; Hydrology (agriculture); Environmental science; Geology; Geography; Geotechnical engineering","score_opus":0.023231491433366492,"score_gpt":0.21727017867531975,"score_spread":0.19403868724195325,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2782247731","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.026783416,0.0012749598,0.0027160828,0.00016158144,0.0001510109,0.0014229998,0.00011795011,0.000064180545,0.9673078],"genre_scores_gemma":[0.48312992,0.0057719955,0.1104787,0.0014040818,0.0002236961,0.0001919216,0.00016268494,0.00022841292,0.3984086],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99616253,0.00016321728,0.0011876568,0.0008111022,0.0010098211,0.0006656865],"domain_scores_gemma":[0.9977674,0.0001967544,0.001058203,0.00075420283,0.000005725362,0.00021770308],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00093936117,0.00058175426,0.0012188331,0.00004587453,0.00007212004,0.0000045119245,0.00058446935,0.0007687008,0.014764714],"category_scores_gemma":[0.0000317929,0.0005179207,0.00092406676,0.000039322465,0.0043627233,0.00007975062,0.00094455533,0.00069027266,0.0006550969],"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":[0.00035532404,0.0028318649,0.03332058,0.0007870814,0.0022110792,0.00007900935,0.0074064382,0.004368622,0.09927552,0.0137975225,0.021515504,0.81405145],"study_design_scores_gemma":[0.0011281819,0.00092167745,0.036618385,0.00016244124,0.00043358194,0.000015359954,0.0001906962,0.00028506477,0.003016506,0.016945887,0.93885106,0.0014311466],"about_ca_topic_score_codex":0.00019835698,"about_ca_topic_score_gemma":0.0000032978899,"teacher_disagreement_score":0.91733557,"about_ca_system_score_codex":0.0003998139,"about_ca_system_score_gemma":0.00001178016,"threshold_uncertainty_score":0.99972725},"labels":[],"label_agreement":null},{"id":"W2782353004","doi":"","title":"Response of brachiopod communities to rapid global climate change during the Ordovician mass extinction, Anticosti Island, Quebec","year":2008,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":0,"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":"Ordovician; Extinction event; Extinction (optical mineralogy); Paleontology; Geology; Climate change; Oceanography; Population; Demography","score_opus":0.02642727082136789,"score_gpt":0.22231187977531258,"score_spread":0.1958846089539447,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2782353004","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.2177076,0.008005014,0.00010780224,0.0012820506,0.00023718188,0.00082279526,0.0014885163,0.000104545885,0.7702445],"genre_scores_gemma":[0.9894398,0.0025417919,0.0019072151,0.0015984804,0.00013742768,0.00000816121,0.000048909213,0.000005059297,0.00431316],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99807566,0.00025869487,0.0005388757,0.00029751903,0.00035181033,0.00047746088],"domain_scores_gemma":[0.99834794,0.0004958116,0.0004954379,0.0004356662,0.00009324752,0.00013188827],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00037375608,0.0003700777,0.00072875427,0.000043719163,0.00062790426,0.000016969238,0.00058100047,0.0004415259,0.00073254906],"category_scores_gemma":[0.000022599968,0.00025459984,0.0005594213,0.000062238374,0.0025526045,0.00005064557,0.000028275768,0.0005129194,0.000019263734],"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":[0.0056263898,0.00008608216,0.5072488,0.00030540818,0.0009093417,0.00007912359,0.010737641,0.000088248235,0.00009277129,0.001192916,0.0019740702,0.47165915],"study_design_scores_gemma":[0.00027032496,0.00069439446,0.97053736,0.00008922797,0.000055062803,0.000044192882,0.0011556844,0.000044951834,0.000007359361,0.00057193934,0.026218345,0.0003111535],"about_ca_topic_score_codex":0.006296214,"about_ca_topic_score_gemma":0.0146739,"teacher_disagreement_score":0.7717322,"about_ca_system_score_codex":0.000010122525,"about_ca_system_score_gemma":0.000063607564,"threshold_uncertainty_score":0.99999064},"labels":[],"label_agreement":null},{"id":"W2787812976","doi":"10.1130/2018.2534(10)","title":"Styles of underplating in the Marin Headlands terrane, Franciscan complex, California","year":2018,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Archaeology and Natural History","field":"Social 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":"McGill University","funders":"","keywords":"Terrane; Underplating; Geology; Seismology; Tectonics","score_opus":0.04540205443072883,"score_gpt":0.2837899569072506,"score_spread":0.23838790247652178,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2787812976","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0026924585,0.0010378645,0.00020794682,0.001002117,0.000075896445,0.0003907013,0.00006133315,0.000040610987,0.9944911],"genre_scores_gemma":[0.82841986,0.001300303,0.011470575,0.0051776543,0.00058960565,0.000023312214,0.00008878462,0.000037367758,0.15289252],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99811685,0.00022480566,0.0004997479,0.0003114952,0.00047335,0.00037373372],"domain_scores_gemma":[0.9984043,0.0006922261,0.00051122834,0.000236429,0.00009097798,0.00006482135],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008229541,0.00023741013,0.0006474651,0.000042332733,0.00038509443,0.0000016832606,0.00062301033,0.00066510757,0.0017781907],"category_scores_gemma":[0.00006062233,0.0001626384,0.00042849893,0.00004525714,0.010461804,0.000017795086,0.00019202275,0.00073168374,0.000019048528],"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":[0.0005935686,0.0002598853,0.017430298,0.00045082392,0.0006864088,0.000045496476,0.24364139,0.000017499451,0.00025005196,0.17191939,0.14971954,0.41498566],"study_design_scores_gemma":[0.00033553652,0.00042065335,0.005278214,0.00010206794,0.000053276515,0.000003578974,0.007516174,0.000051173636,0.0000039402416,0.10846462,0.8774094,0.0003613624],"about_ca_topic_score_codex":0.0024389394,"about_ca_topic_score_gemma":0.0011525295,"teacher_disagreement_score":0.8415986,"about_ca_system_score_codex":0.00008215077,"about_ca_system_score_gemma":0.00011553064,"threshold_uncertainty_score":0.9991343},"labels":[],"label_agreement":null},{"id":"W2886742252","doi":"","title":"Use of Whirlpool Sandstone Silurian as a building stone in southern Ontario","year":2008,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":0,"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":"Geology; Archaeology; Paleontology; Mining engineering; Geography","score_opus":0.04463244282884888,"score_gpt":0.2372077258657948,"score_spread":0.19257528303694593,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2886742252","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6667597,0.000938191,0.000029638108,0.00024572454,0.00009335256,0.0005086317,0.000108908316,0.00004458165,0.33127123],"genre_scores_gemma":[0.6657319,0.00065108587,0.007402737,0.0008479855,0.000060474547,0.0000047126596,0.0001682812,0.00001602051,0.32511678],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9975635,0.00011526572,0.00068944244,0.00057858037,0.00043791527,0.000615317],"domain_scores_gemma":[0.99816114,0.00071448006,0.00048694352,0.00036611813,0.00010069657,0.00017062998],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002855434,0.0003942822,0.001164415,0.000112488466,0.00014520125,0.000008355154,0.00043419717,0.0010091154,0.00792988],"category_scores_gemma":[0.000053799573,0.00032436213,0.0005243059,0.00005256754,0.0032212068,0.00004400828,0.000097166514,0.001311181,0.00021417002],"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":[0.0003010476,0.000038389888,0.98689216,0.000060647842,0.00022271542,0.00011904789,0.0049485876,0.00029335584,0.000018079689,0.00023947991,0.0007136166,0.0061528976],"study_design_scores_gemma":[0.0039846655,0.006500564,0.66835064,0.00087413396,0.00040586627,0.0010010519,0.003180383,0.001465671,0.00016894937,0.026705496,0.2839401,0.0034224407],"about_ca_topic_score_codex":0.06780627,"about_ca_topic_score_gemma":0.033713844,"teacher_disagreement_score":0.31854147,"about_ca_system_score_codex":0.000009971314,"about_ca_system_score_gemma":0.00028779023,"threshold_uncertainty_score":0.99992085},"labels":[],"label_agreement":null},{"id":"W2913425250","doi":"","title":"Hydrochemical and isotopic variability of cave drip water with increasing elevation, Vancouver Island, Canada","year":2008,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Karst Systems and Hydrogeology","field":"Earth and Planetary Sciences","cited_by":0,"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":"Elevation (ballistics); Cave; Hydrology (agriculture); Geology; Archaeology; Physical geography; Geography","score_opus":0.006347228557494573,"score_gpt":0.15367497084178364,"score_spread":0.14732774228428908,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2913425250","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5575864,0.00035797962,0.00036180284,0.00012427654,0.00016590084,0.00057165703,0.00021143873,0.000045778223,0.4405748],"genre_scores_gemma":[0.9810328,0.00007231604,0.0013375999,0.00052492844,0.000084580664,0.0000016867536,0.00009660058,0.0000072764924,0.016842203],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99835,0.00006344193,0.0004906109,0.0004265426,0.00034533613,0.00032404027],"domain_scores_gemma":[0.9989445,0.0002881759,0.00030078756,0.00023126209,0.0001113108,0.00012392428],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00019649445,0.0002889448,0.00078383397,0.0000181974,0.000113942464,0.0000040260516,0.00015231,0.00036579143,0.001077122],"category_scores_gemma":[0.000017132183,0.00017656307,0.00016495166,0.000015620066,0.0012762266,0.000022257922,0.000045469034,0.0003333643,0.0000024989283],"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":[0.00051839044,0.000053619406,0.952078,0.00082050014,0.0012012322,0.00007913209,0.0026369388,0.00027700484,0.00033148137,0.0005501246,0.031010596,0.010443008],"study_design_scores_gemma":[0.0032781502,0.00336451,0.1623926,0.00051737914,0.0007210597,0.00063077785,0.00085750356,0.0061875945,0.0009984355,0.012511529,0.80522716,0.003313268],"about_ca_topic_score_codex":0.3407059,"about_ca_topic_score_gemma":0.116037905,"teacher_disagreement_score":0.78968537,"about_ca_system_score_codex":0.000017537122,"about_ca_system_score_gemma":0.00017378633,"threshold_uncertainty_score":0.999836},"labels":[],"label_agreement":null},{"id":"W2946848879","doi":"10.1130/2019.2536(15)","title":"Interpretation of mouth-bar and related lacustrine and fluvial sand bodies from the middle Green River Formation (Eocene), southern Uinta Basin, Utah","year":2019,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological formations and processes","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 New Brunswick","funders":"Universitetet i Bergen","keywords":"Fluvial; Geology; Tributary; Marine transgression; Paleontology; Canyon; Structural basin; River mouth; Geomorphology; Geography; Sediment","score_opus":0.01856465431088197,"score_gpt":0.18568947129930705,"score_spread":0.16712481698842507,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2946848879","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6827063,0.006848084,0.0011226776,0.0012604824,0.00019573151,0.001164095,0.0025887364,0.000108786626,0.30400512],"genre_scores_gemma":[0.9754604,0.0007694822,0.0013636387,0.0004840583,0.00004204881,0.0000012792992,0.0004929854,0.000005417628,0.021380663],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99884665,0.000058797712,0.00045488242,0.00024886968,0.0002192708,0.00017154441],"domain_scores_gemma":[0.99867916,0.00052996294,0.0004873951,0.00014701243,0.000098691,0.000057775233],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00020131776,0.00023383464,0.0004632052,0.000021104095,0.00014767077,0.000022909384,0.00017470524,0.0003104606,0.0015389574],"category_scores_gemma":[0.00003598822,0.00013698508,0.00016260643,0.00001965867,0.001263858,0.000093992225,0.00007880627,0.00029466403,0.000047001413],"study_design_candidate":"design_other","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":[0.0006293848,0.0000273629,0.03726105,0.00047551683,0.0006348755,0.0000029169469,0.034901552,0.00033640515,0.000031311825,0.0014252225,0.0010610657,0.92321336],"study_design_scores_gemma":[0.004007331,0.0037591709,0.34500375,0.0012827592,0.0015508297,0.00009170797,0.020123431,0.053473093,0.0001815084,0.4830373,0.08499488,0.002494232],"about_ca_topic_score_codex":0.0018290732,"about_ca_topic_score_gemma":0.000040641393,"teacher_disagreement_score":0.9207191,"about_ca_system_score_codex":0.0000032235776,"about_ca_system_score_gemma":0.0000221634,"threshold_uncertainty_score":0.9993738},"labels":[],"label_agreement":null},{"id":"W2948289229","doi":"10.1130/2020.2548(13)","title":"Glaciers, isostasy, and eustasy in the Fraser Lowland: A new interpretation of late Pleistocene glaciation across the International Boundary","year":2020,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geology and Paleoclimatology Research","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":"Simon Fraser University","funders":"","keywords":"Geology; Meltwater; Subaerial; Ice sheet; Glacier; Paleontology; Deglaciation; Radiocarbon dating; Sea level; Physical geography; Pleistocene; Glacial period; Moraine; Sedimentary depositional environment; Oceanography; Geomorphology; Geography","score_opus":0.019326306762267386,"score_gpt":0.24755414459007055,"score_spread":0.22822783782780318,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2948289229","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.3782634,0.0073177563,0.0015274183,0.030495552,0.00055475894,0.0019184792,0.00073158654,0.00007550053,0.5791155],"genre_scores_gemma":[0.98857224,0.00054767594,0.000480502,0.0035435255,0.00007150173,0.0000027335045,0.00026695107,0.000004142008,0.0065107485],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986075,0.00011780684,0.00038646813,0.00030239113,0.00034234644,0.00024349356],"domain_scores_gemma":[0.9985346,0.0008386229,0.0003388427,0.00016639983,0.00006175651,0.000059767583],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00051364355,0.00019182728,0.00038392685,0.00002351914,0.00015417424,0.000027859463,0.00051594764,0.00032161162,0.00064180914],"category_scores_gemma":[0.00007826052,0.00011185179,0.00018997528,0.000041945998,0.0017694915,0.000040417704,0.00009599981,0.0007138773,0.000025379148],"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":[0.0006954997,0.000016142365,0.9035883,0.00007901237,0.00026989993,0.000019284802,0.009530559,0.00015445917,0.0000028092466,0.001067751,0.003932963,0.080643296],"study_design_scores_gemma":[0.0020103506,0.0018410153,0.75140584,0.00016596819,0.00015249844,0.00006049598,0.0055505056,0.022233985,0.000018478866,0.07809722,0.13777794,0.00068569643],"about_ca_topic_score_codex":0.0004913474,"about_ca_topic_score_gemma":0.00066519756,"teacher_disagreement_score":0.6103088,"about_ca_system_score_codex":0.0000041894905,"about_ca_system_score_gemma":0.00010423884,"threshold_uncertainty_score":0.70273596},"labels":[],"label_agreement":null},{"id":"W2957119960","doi":"10.1130/2018.0051(08)","title":"Lake level, shoreline, and dune behavior along the Indiana southern shore of Lake Michigan","year":2018,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Hydrology and Sediment Transport Processes","field":"Environmental 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":"University of Waterloo","funders":"","keywords":"Shore; Oceanography; Geology; Hydrology (agriculture); Geography; Physical geography; Geotechnical engineering","score_opus":0.02019237602217646,"score_gpt":0.21572705371329948,"score_spread":0.195534677691123,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2957119960","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.65936136,0.0007777257,0.0005878866,0.0014767727,0.00016407178,0.0015314996,0.0013738914,0.0001444813,0.3345823],"genre_scores_gemma":[0.89066863,0.00043626162,0.003434588,0.0028788836,0.00016031075,0.000048916703,0.0002359418,0.000060921662,0.10207558],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9982384,0.000026841057,0.0005143972,0.00051076146,0.00037595333,0.00033364445],"domain_scores_gemma":[0.9990368,0.00011293365,0.00038819542,0.00032701838,0.000027584385,0.00010749864],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00024823652,0.00036402978,0.0005961805,0.000014642749,0.0001680812,0.0000066688385,0.00046771363,0.0005387548,0.012483651],"category_scores_gemma":[0.000009254391,0.000236928,0.0003260862,0.00002971201,0.0066141877,0.000025268133,0.00025246336,0.00055402744,0.00007888319],"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":[0.0007458117,0.00101658,0.52796835,0.0007509159,0.002403084,0.00017535049,0.08588244,0.00015616142,0.0037532016,0.0013330213,0.024158223,0.35165685],"study_design_scores_gemma":[0.0012911486,0.002597321,0.10922543,0.00023244508,0.0015070024,0.000056300196,0.0023350646,0.0001383366,0.0006632305,0.012516623,0.86754227,0.0018948503],"about_ca_topic_score_codex":0.00011023677,"about_ca_topic_score_gemma":0.0026837585,"teacher_disagreement_score":0.843384,"about_ca_system_score_codex":0.000006055987,"about_ca_system_score_gemma":0.000023045102,"threshold_uncertainty_score":0.9960892},"labels":[],"label_agreement":null},{"id":"W2958080237","doi":"10.1130/2019.0052(02)","title":"The science and industry of the Permian Hutchinson Salt","year":2019,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":"","keywords":"Permian; Environmental ethics; Geology; Philosophy; Paleontology","score_opus":0.013845536346933437,"score_gpt":0.19097735773964428,"score_spread":0.17713182139271083,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2958080237","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.1483192,0.0011354679,0.000005354655,0.0026966075,0.00013165173,0.0003222671,0.00007681531,0.000024293857,0.8472883],"genre_scores_gemma":[0.9048262,0.00031414724,0.0003865748,0.001645028,0.00006941972,8.536958e-7,0.000008686274,0.0000038059109,0.09274523],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9979851,0.000037714166,0.00039191384,0.00044559478,0.0007615049,0.00037816536],"domain_scores_gemma":[0.9983404,0.0004499549,0.00046418398,0.0004194731,0.00019075001,0.00013520457],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00046706773,0.00025341375,0.00050630816,0.000017788001,0.00044222947,0.000027786884,0.0009395018,0.0004672137,0.0016329269],"category_scores_gemma":[0.00013312056,0.000109104505,0.0004371997,0.00009914828,0.0088491095,0.000025043824,0.00028011028,0.0009991742,0.000025141959],"study_design_candidate":"design_other","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":[0.00016596275,0.00006368513,0.19743301,0.00026235665,0.000663933,0.00000532532,0.00095006934,0.0004102735,0.0015984263,0.034239594,0.0072453953,0.75696194],"study_design_scores_gemma":[0.0005110584,0.0011856155,0.34768495,0.0001989328,0.0004166752,0.00003157904,0.0010907904,0.0037505385,0.0010050654,0.2812754,0.36168075,0.0011686679],"about_ca_topic_score_codex":0.00075194845,"about_ca_topic_score_gemma":0.000047779642,"teacher_disagreement_score":0.75650704,"about_ca_system_score_codex":0.000006658399,"about_ca_system_score_gemma":0.00015486748,"threshold_uncertainty_score":0.99927974},"labels":[],"label_agreement":null},{"id":"W2979334553","doi":"10.1130/2018.2541(28)","title":"Latest Cretaceous–early Eocene Pacific-Arctic?-Atlantic connection: Co-evolution of strike-slip fault systems, oroclines, and transverse fold-and-thrust belts in the northwestern North American Cordillera","year":2019,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":true,"ca_institutions":"Yukon University","funders":"","keywords":"Geology; Paleontology; Transform fault; Plate tectonics; Cretaceous; Thrust fault; Paleogene; Seafloor spreading; Arctic; North American Plate; Rift; Seismology; Fault (geology); Oceanography; Tectonics","score_opus":0.013794742790514293,"score_gpt":0.19217193650803857,"score_spread":0.17837719371752428,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2979334553","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97074276,0.001493941,0.00007796831,0.0004511209,0.000063201725,0.0006953476,0.00039466858,0.000044131208,0.026036877],"genre_scores_gemma":[0.9954509,0.0013699423,0.000173876,0.0002523775,0.00007646851,0.000004401365,0.0003640871,0.000008196244,0.002299743],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9972778,0.00014441572,0.00082649355,0.0007194223,0.00056082284,0.00047102864],"domain_scores_gemma":[0.9977386,0.000820718,0.0007624807,0.00033311071,0.00017465661,0.0001704102],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00026475015,0.00049722416,0.0013842883,0.00007030927,0.00015749139,0.000038519596,0.0003522786,0.00034148776,0.0006591706],"category_scores_gemma":[0.000029967263,0.00030995638,0.00042743303,0.00016252775,0.0019031521,0.000052069587,0.000051643074,0.00069125864,0.000025731859],"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":[0.00018728885,0.000059889444,0.98517925,0.00027660702,0.00033537135,0.000018737734,0.00047250788,0.00047446674,0.000016630416,0.00017003962,0.00014433051,0.012664907],"study_design_scores_gemma":[0.0010075578,0.002706508,0.9739058,0.00017262733,0.0006494909,0.00007250634,0.0035099676,0.0044268514,0.0000058514424,0.0008551793,0.011775423,0.0009122301],"about_ca_topic_score_codex":0.023159513,"about_ca_topic_score_gemma":0.0032763642,"teacher_disagreement_score":0.024708165,"about_ca_system_score_codex":0.000015286148,"about_ca_system_score_gemma":0.0000480075,"threshold_uncertainty_score":0.99993527},"labels":[],"label_agreement":null},{"id":"W2979365870","doi":"10.1130/2018.2541(26)","title":"Unravelling the thermal evolution of the Neruokpuk Formation in the British Mountains, North Yukon, Canada: Tectonic and orogenic implications","year":2019,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological Studies and Exploration","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":"Zircon; Geology; Fission track dating; Paleontology; Thermochronology; Basement; Arctic; Geodynamics; Proterozoic; Subduction; Cretaceous; Tectonics; Oceanography; Archaeology; Geography","score_opus":0.014562281386371691,"score_gpt":0.16957311351863344,"score_spread":0.15501083213226174,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2979365870","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.81031,0.007544796,0.00071767595,0.007393984,0.00021528424,0.0025045492,0.00035233682,0.000035364883,0.17092599],"genre_scores_gemma":[0.9963282,0.00072647934,0.000063347914,0.0010293827,0.00004209869,0.0000060745447,0.00006280194,0.000002954986,0.0017386972],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99876577,0.00007875643,0.00038874382,0.00021927035,0.00030416713,0.00024327698],"domain_scores_gemma":[0.9989664,0.0002865548,0.00040003113,0.00024025881,0.00008030709,0.000026458009],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021864632,0.00016744297,0.0002857061,0.000007217653,0.0005627062,0.000032902135,0.00040458588,0.00014891378,0.00009564388],"category_scores_gemma":[0.000022416292,0.00008293242,0.00018016332,0.0000658569,0.0006819813,0.00003676799,0.00007241643,0.0003792738,0.0000037057084],"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":[0.0001346431,0.000079656165,0.5717477,0.00038122566,0.0005665463,0.0000060382818,0.00669529,0.034424417,0.0000827972,0.017872639,0.013559237,0.3544498],"study_design_scores_gemma":[0.00014853582,0.0001611499,0.9695661,0.000036672554,0.00005813021,0.000018340525,0.0018146462,0.0026972792,0.0000025788368,0.0050215004,0.020292554,0.00018251946],"about_ca_topic_score_codex":0.2962251,"about_ca_topic_score_gemma":0.46797517,"teacher_disagreement_score":0.3978184,"about_ca_system_score_codex":0.00003378653,"about_ca_system_score_gemma":0.00012852692,"threshold_uncertainty_score":0.7084614},"labels":[],"label_agreement":null},{"id":"W2979485598","doi":"10.1130/2018.2541(16)","title":"Paleogene sedimentation and Eurekan deformation in the Stenkul Fiord area of southeastern Ellesmere Island (Canadian Arctic): Evidence for a polyphase history","year":2019,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological Studies and Exploration","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":"","keywords":"Geology; Unconformity; Paleogene; Paleontology; Clastic rock; Sedimentary rock; Sedimentary depositional environment; Geochemistry; Structural basin","score_opus":0.06525030373032166,"score_gpt":0.22431726398744348,"score_spread":0.1590669602571218,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2979485598","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.3309794,0.034962445,0.0042802407,0.0135376295,0.0009687089,0.010833757,0.0027705021,0.00009885722,0.60156846],"genre_scores_gemma":[0.9902569,0.0009701382,0.00076374714,0.0023255995,0.0000506524,0.000009873982,0.00032282333,0.000004657394,0.0052956115],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9988568,0.000047349124,0.0003779797,0.00025532334,0.00022615497,0.0002363982],"domain_scores_gemma":[0.9989401,0.0004046766,0.00036305893,0.00013815182,0.00008359238,0.00007042009],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002985056,0.0001959824,0.00037318488,0.0000360091,0.000093842325,0.000009460048,0.00016718521,0.00020952917,0.0007076371],"category_scores_gemma":[0.000037211943,0.00012266314,0.00018332961,0.00001963327,0.00045322155,0.00005560561,0.000019030826,0.00018228868,0.000009794897],"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":[0.0018438053,0.000103304505,0.24765682,0.0016364036,0.0006113832,0.000013173626,0.030664857,0.0022133635,0.000101817524,0.0024151679,0.00785178,0.7048881],"study_design_scores_gemma":[0.0040315907,0.010509691,0.46943995,0.0013632098,0.0007193464,0.000041925297,0.0255045,0.023800187,0.000029394814,0.01883795,0.44362903,0.0020932073],"about_ca_topic_score_codex":0.014084199,"about_ca_topic_score_gemma":0.029436557,"teacher_disagreement_score":0.7027949,"about_ca_system_score_codex":0.000017881266,"about_ca_system_score_gemma":0.00007783467,"threshold_uncertainty_score":0.9924811},"labels":[],"label_agreement":null},{"id":"W2979532019","doi":"10.1130/2018.2541(07)","title":"Late Cretaceous–Paleogene burial and exhumation history of the Southwestern Basement Province, Svalbard, revealed by zircon (U-Th)/He thermochronology","year":2019,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological Studies and Exploration","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 Ottawa","funders":"","keywords":"Geology; Thermochronology; Cretaceous; Zircon; Rift; Paleontology; Paleogene; Basement; Tectonics; Geomorphology; Geochemistry; Geography; Archaeology","score_opus":0.01756734600372261,"score_gpt":0.17545493595544567,"score_spread":0.15788758995172306,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2979532019","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.123787075,0.022584675,0.0010249281,0.0020599216,0.0013464992,0.0029971525,0.00050389534,0.00012897456,0.84556687],"genre_scores_gemma":[0.4800457,0.0060702264,0.0022939788,0.0035099396,0.0004429666,0.000020494284,0.00063446566,0.00003553892,0.5069467],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.998211,0.00010461268,0.0005456897,0.00047809893,0.0003535102,0.0003070643],"domain_scores_gemma":[0.99855185,0.00017202251,0.00082667253,0.00029835658,0.0000819585,0.00006915491],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002328154,0.0003333002,0.0007110125,0.000016929898,0.00012179418,0.000008712474,0.0003004455,0.00044906719,0.003593624],"category_scores_gemma":[0.000018684512,0.00020225247,0.0003587036,0.000015075119,0.0014934243,0.000032611235,0.00013601508,0.00033930576,0.000044065895],"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":[0.0017026375,0.00020724071,0.060551416,0.0014592195,0.0025722932,0.000013620734,0.0065495037,0.0013742633,0.0053272126,0.0014530136,0.09301625,0.82577336],"study_design_scores_gemma":[0.0015518733,0.002911342,0.035365485,0.00017231565,0.00042335317,0.00000804214,0.0004875988,0.0015038941,0.00012755851,0.004724245,0.9517686,0.0009556987],"about_ca_topic_score_codex":0.00035985344,"about_ca_topic_score_gemma":0.00007477652,"teacher_disagreement_score":0.85875237,"about_ca_system_score_codex":0.000036386005,"about_ca_system_score_gemma":0.0001012476,"threshold_uncertainty_score":0.99731725},"labels":[],"label_agreement":null},{"id":"W2979558319","doi":"10.1130/2018.2541(18)","title":"Structural evidence for sinistral displacement on the Wegener Fault in southern Nares Strait, Arctic Canada","year":2019,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological Studies and Exploration","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":"","keywords":"Sinistral and dextral; Geology; Transform fault; Fault (geology); Seismology; Paleontology; Arctic; Metamorphism; Oceanography","score_opus":0.06016860981784824,"score_gpt":0.23286580887633657,"score_spread":0.17269719905848832,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2979558319","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5458445,0.0052739168,0.00042278768,0.03308509,0.0019976534,0.008594308,0.00526596,0.00014393347,0.39937186],"genre_scores_gemma":[0.9481392,0.00012386023,0.00033915776,0.002717167,0.00012218824,0.000009988578,0.00017442043,0.00000617651,0.048367877],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9982635,0.000041481813,0.00038591123,0.00043042094,0.00042471132,0.00045398436],"domain_scores_gemma":[0.9984054,0.0009622368,0.00029512757,0.00020197622,0.00006618789,0.000069081136],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00018516352,0.00031569455,0.0004665142,0.000009325932,0.00020563033,0.000020795424,0.00033814684,0.00020211852,0.0016451643],"category_scores_gemma":[0.00006572606,0.00016897163,0.00029025186,0.000019290977,0.0005322417,0.000019372756,0.0000461146,0.00038719148,0.000028228545],"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":[0.0050844206,0.00012991391,0.20901741,0.0017798418,0.0025594363,0.00006314503,0.009882881,0.12094019,0.0000698589,0.0588683,0.08513191,0.50647265],"study_design_scores_gemma":[0.003236141,0.015290154,0.33182982,0.0018013858,0.00054215384,0.000019497464,0.036305945,0.039793883,0.00004172582,0.113353066,0.45266446,0.00512177],"about_ca_topic_score_codex":0.21413943,"about_ca_topic_score_gemma":0.22800109,"teacher_disagreement_score":0.5013509,"about_ca_system_score_codex":0.000038461632,"about_ca_system_score_gemma":0.00015674479,"threshold_uncertainty_score":0.99926746},"labels":[],"label_agreement":null},{"id":"W2979666414","doi":"10.1130/2018.2541(24)","title":"Geochemical constraints on the provenance of pre-Mississippian sedimentary rocks in the North Slope subterrane of Yukon and Alaska","year":2019,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological Studies and Exploration","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":"Yukon University","funders":"","keywords":"Laurentia; Geology; Provenance; Terrane; Paleozoic; Devonian; Ordovician; Sedimentary rock; Paleontology; Tectonics","score_opus":0.021328395559773134,"score_gpt":0.1948823717285712,"score_spread":0.17355397616879806,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2979666414","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.53583336,0.0011391924,0.000055200766,0.0038158076,0.00009562823,0.0015453919,0.00029900193,0.00001984182,0.45719656],"genre_scores_gemma":[0.99461657,0.0005702162,0.00024402035,0.0017116742,0.00003681677,0.000004125934,0.00008955472,0.0000033995072,0.002723602],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99847305,0.00006800014,0.00048271107,0.0003394562,0.0003812754,0.00025552974],"domain_scores_gemma":[0.99857175,0.00061829796,0.0004764672,0.00023590647,0.000050229988,0.000047315236],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00025816535,0.00025736773,0.0005946838,0.000013822527,0.00008588886,0.00000681339,0.00034377354,0.00023365302,0.0009929652],"category_scores_gemma":[0.00003356366,0.00012427813,0.00023271426,0.000034909797,0.0020758624,0.00001990002,0.00007112309,0.0004536213,0.0000072482467],"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":[0.0014666957,0.00032361876,0.32715827,0.0007835507,0.0007511554,0.000020455478,0.01141875,0.0014559444,0.0001841496,0.0033231617,0.012848725,0.6402655],"study_design_scores_gemma":[0.0014682205,0.00695127,0.9120474,0.00067861995,0.00022801226,0.00002235209,0.005350949,0.0016082077,0.00031570022,0.017211378,0.05307419,0.001043703],"about_ca_topic_score_codex":0.00048209738,"about_ca_topic_score_gemma":0.000060800776,"teacher_disagreement_score":0.63922185,"about_ca_system_score_codex":0.0000044227954,"about_ca_system_score_gemma":0.000030406178,"threshold_uncertainty_score":0.99992025},"labels":[],"label_agreement":null},{"id":"W2979669984","doi":"10.1130/2018.2541(15)","title":"Early Cretaceous magmatism and post-Early Cretaceous deformation on Ellef Ringnes Island, Canadian High Arctic, related to the formation of the Arctic Ocean","year":2019,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","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":"","keywords":"Geology; Dike; Sill; Sinistral and dextral; Continental margin; Cretaceous; Paleontology; Mantle plume; Arctic; Large igneous province; Magmatism; Seismology; Geochemistry; Fault (geology); Oceanography; Lithosphere; Tectonics","score_opus":0.006453748668444654,"score_gpt":0.16526990259059254,"score_spread":0.1588161539221479,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2979669984","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.90161103,0.0005633105,0.000039427545,0.0057349843,0.0001504115,0.0010573812,0.000597744,0.00003582238,0.09020988],"genre_scores_gemma":[0.9772621,0.00013119579,0.00024243204,0.0024468862,0.000031564923,0.0000018307172,0.00021951008,0.0000069321045,0.019657584],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99795365,0.00009493009,0.0006160991,0.00037931406,0.00051510637,0.00044089172],"domain_scores_gemma":[0.99824303,0.0003671948,0.000544226,0.0004032526,0.0002156307,0.00022666204],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000258594,0.00036363673,0.00061971653,0.00006300578,0.00030555576,0.000043768538,0.0005030881,0.0004184367,0.0030011737],"category_scores_gemma":[0.00009421855,0.0001852403,0.00047827023,0.00009310215,0.0006855186,0.00006493961,0.00009510326,0.00065622356,0.00021859907],"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":[0.0016660481,0.00022070657,0.30841905,0.0024030372,0.00391644,0.00006147363,0.03454064,0.030605892,0.0004452705,0.021702157,0.01010258,0.5859167],"study_design_scores_gemma":[0.000979651,0.004502294,0.8090581,0.0005418946,0.00086982927,0.00010340682,0.0010797393,0.008149922,0.00014088403,0.12137886,0.05166899,0.0015263914],"about_ca_topic_score_codex":0.09919148,"about_ca_topic_score_gemma":0.022620333,"teacher_disagreement_score":0.58439034,"about_ca_system_score_codex":0.000025195057,"about_ca_system_score_gemma":0.00005694142,"threshold_uncertainty_score":0.9979102},"labels":[],"label_agreement":null},{"id":"W2979835434","doi":"10.1130/2018.2541(08)","title":"40Ar/39Ar geochronologic evidence of Eurekan deformation within the West Spitsbergen Fold and Thrust Belt","year":2019,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","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 Ottawa","funders":"","keywords":"Geology; Greenschist; Mylonite; Metamorphism; Geochemistry; Shear zone; Metamorphic facies; Muscovite; Geochronology; Metamorphic rock; Paleontology; Tectonics; Quartz; Facies","score_opus":0.021383476997813476,"score_gpt":0.19936808013231705,"score_spread":0.17798460313450357,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2979835434","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.23989472,0.013152727,0.00026294842,0.0032308968,0.00020290747,0.0011639396,0.00022753881,0.00013498215,0.7417293],"genre_scores_gemma":[0.97778875,0.001530806,0.0017644782,0.0014486746,0.00007670151,0.000002678467,0.00012577114,0.0000061679907,0.017255956],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99768364,0.000079344616,0.0007745395,0.0005556605,0.0005205345,0.00038625387],"domain_scores_gemma":[0.9976153,0.0006936294,0.0009740359,0.00042619565,0.00015440963,0.0001364428],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00046027676,0.0004288398,0.00093850977,0.000033803204,0.00018426262,0.000022412873,0.00062277564,0.00054216536,0.0076415427],"category_scores_gemma":[0.00010370265,0.00022758415,0.00062151806,0.000073651834,0.0022341255,0.00007655686,0.00020623271,0.0006676801,0.00014850276],"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":[0.0011548452,0.00026982604,0.33685848,0.0030137494,0.0041656503,0.000040765666,0.004380783,0.008785427,0.0025756625,0.04892024,0.007943552,0.581891],"study_design_scores_gemma":[0.001619124,0.0102738645,0.48671287,0.0015765579,0.0027899703,0.00013287003,0.0032185891,0.023559047,0.0013722152,0.40832385,0.056285195,0.0041358373],"about_ca_topic_score_codex":0.0017089918,"about_ca_topic_score_gemma":0.00017436195,"teacher_disagreement_score":0.73789406,"about_ca_system_score_codex":0.000007812217,"about_ca_system_score_gemma":0.000060767776,"threshold_uncertainty_score":0.9932656},"labels":[],"label_agreement":null},{"id":"W2979852859","doi":"10.1130/2018.2541(27)","title":"Evidence for subtropical warmth in the Canadian Arctic (Beaufort-Mackenzie, Northwest Territories, Canada) during the early Eocene","year":2019,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","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":"Arctic; Geology; Oceanography; Paleogene; Arctic dipole anomaly; Arctic ecology; Subtropics; Canada Basin; Latitude; Cenozoic; Structural basin; Paleontology; Arctic ice pack; Ecology","score_opus":0.038569787115610925,"score_gpt":0.23444090558273603,"score_spread":0.1958711184671251,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2979852859","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.74753517,0.006559608,0.000022705986,0.02281592,0.0014201608,0.0053146696,0.0021861305,0.00006884606,0.2140768],"genre_scores_gemma":[0.983056,0.00022533446,0.00016942319,0.0022308943,0.00017386659,0.000015641865,0.0002313986,0.000007656041,0.0138897635],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99743706,0.00014520323,0.00044617636,0.0005103404,0.00056151004,0.00089969067],"domain_scores_gemma":[0.99676824,0.0021761288,0.00023140029,0.00048147223,0.00014722094,0.00019554551],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00049164187,0.0003400106,0.0005896676,0.00004157687,0.0006475965,0.00003707515,0.0011073815,0.00056809,0.00068018824],"category_scores_gemma":[0.00014053883,0.00019455994,0.00031072515,0.00005695971,0.0019329634,0.00003823883,0.000052621483,0.0013223303,0.000021887749],"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":[0.00008184206,0.0000037026823,0.997313,0.000098244156,0.00006979145,0.000035036934,0.00028340652,0.000046039084,1.5227734e-7,0.0007293881,0.00046401884,0.00087533204],"study_design_scores_gemma":[0.00021438909,0.00031665596,0.9555347,0.000079629,0.000041184347,0.00004712242,0.0001829483,0.00011971761,0.0000011901412,0.0018839203,0.041320156,0.00025839522],"about_ca_topic_score_codex":0.9773908,"about_ca_topic_score_gemma":0.99873155,"teacher_disagreement_score":0.23552087,"about_ca_system_score_codex":0.000043558706,"about_ca_system_score_gemma":0.0018091227,"threshold_uncertainty_score":0.79339236},"labels":[],"label_agreement":null},{"id":"W2979895441","doi":"10.1130/2018.2540(28)","title":"Provenance of Permian eolian and related strata in the North American midcontinent: Tectonic and climatic controls on sediment dispersal in western tropical Pangea","year":2018,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":7,"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; University of Oklahoma; University of Arizona; West Virginia University; National Science Foundation","keywords":"Geology; Laurentia; Provenance; Permian; Paleontology; Gondwana; Paleozoic; Siliciclastic; Red beds; Paleocurrent; Supercontinent; Pangaea; Sedimentary rock; Craton; Sedimentary depositional environment; Clastic rock; Tectonics; Structural basin","score_opus":0.013461124417744318,"score_gpt":0.2124677226715841,"score_spread":0.19900659825383976,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2979895441","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9190109,0.0017542021,0.0000047294434,0.0006276792,0.00002789181,0.00062010385,0.000114137074,0.00001272395,0.07782764],"genre_scores_gemma":[0.998503,0.00044690908,0.0002643674,0.00027518513,0.000023376555,0.000005346842,0.000015897007,0.0000022848428,0.00046363208],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983118,0.00012543089,0.000540722,0.00043159162,0.00024461214,0.00034579652],"domain_scores_gemma":[0.9988553,0.00037823906,0.0004489672,0.00021615613,0.000020109263,0.00008122585],"candidate_categories":["sts"],"consensus_categories":[],"category_scores_codex":[0.00018565307,0.00029295983,0.00080049114,0.00004727749,0.00006970126,0.000014321856,0.00025469606,0.00022270346,0.00006403024],"category_scores_gemma":[0.00001822448,0.00018348994,0.00017430904,0.000049963135,0.0037811496,0.00003083893,0.000010610345,0.00058138615,0.000001884876],"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":[0.00022892562,0.000049680246,0.90873384,0.00008453555,0.00010842927,0.000027141261,0.0025094363,0.000004568262,0.0000061552037,0.0004018262,0.00003877299,0.0878067],"study_design_scores_gemma":[0.0006145,0.0020139527,0.9945746,0.00011605779,0.00004164828,0.000013696508,0.00044762707,0.00044861037,0.0000011366786,0.0011335509,0.0003987396,0.00019587499],"about_ca_topic_score_codex":0.0007526574,"about_ca_topic_score_gemma":0.0050238795,"teacher_disagreement_score":0.087610826,"about_ca_system_score_codex":0.000004477651,"about_ca_system_score_gemma":0.000033145203,"threshold_uncertainty_score":0.99893},"labels":[],"label_agreement":null},{"id":"W2979912456","doi":"10.1130/2018.2541(20)","title":"The Whale Mountain allochthon: A relic of the Iapetus Ocean preserved in the northeastern Brooks Range of Alaska and Yukon","year":2019,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological Studies and Exploration","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":"Yukon University","funders":"","keywords":"Geology; Allochthon; Volcanic rock; Paleontology; Maar; Basalt; Geochemistry; Pyroclastic rock; Volcano; Nappe","score_opus":0.021572804811022802,"score_gpt":0.19154100811181082,"score_spread":0.16996820330078802,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2979912456","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.51573384,0.008078891,0.00002977803,0.005734581,0.00025354404,0.002320858,0.00015759887,0.000031005056,0.46765992],"genre_scores_gemma":[0.97702223,0.0017727026,0.00012466787,0.00092458545,0.00006567716,0.0000036334216,0.000020905902,0.0000057855514,0.020059833],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981715,0.00017103677,0.00054407003,0.00031826994,0.00048420747,0.00031092673],"domain_scores_gemma":[0.9980552,0.00082464016,0.00058580167,0.00040875148,0.00008468458,0.000040918545],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000552318,0.0002621596,0.0005703557,0.000011777433,0.00021364845,0.000018360312,0.0006674036,0.00026394427,0.00018531377],"category_scores_gemma":[0.000051765433,0.000109822235,0.000384521,0.00004512877,0.0018416176,0.00002739319,0.00018330463,0.00045100428,0.000012375314],"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":[0.0012245361,0.00015608603,0.7778339,0.0007828462,0.0008486802,0.000010410658,0.015425516,0.0026571902,0.000035318033,0.00490218,0.00797489,0.18814848],"study_design_scores_gemma":[0.0014149783,0.0029656324,0.77223796,0.0003266436,0.0002236906,0.000017217897,0.009916875,0.0039618197,0.000017907567,0.023979455,0.18421961,0.00071819586],"about_ca_topic_score_codex":0.0019603618,"about_ca_topic_score_gemma":0.00067162624,"teacher_disagreement_score":0.4612884,"about_ca_system_score_codex":0.0000048148304,"about_ca_system_score_gemma":0.00003231491,"threshold_uncertainty_score":0.6785517},"labels":[],"label_agreement":null},{"id":"W2980076769","doi":"10.1130/2018.2541(13)","title":"Early Carboniferous syn-rift sedimentation in the Sverdrup Basin (Yelverton Pass area, northern Ellesmere Island, Arctic Canada): A solution to the Okse Bay problem","year":2019,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":true,"ca_institutions":"Geological Survey of Canada; University of Calgary","funders":"","keywords":"Geology; Carboniferous; Paleontology; Devonian; Unconformity; Sverdrup; Paleozoic; Late Devonian extinction; Bay; Orogeny; Palynology; Clastic rock; Structural basin; Oceanography; Pollen","score_opus":0.00938423510154785,"score_gpt":0.17061685526843828,"score_spread":0.16123262016689044,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2980076769","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6208859,0.00076031085,0.0003171517,0.02677772,0.0002674363,0.0028562213,0.000657442,0.00007689972,0.34740087],"genre_scores_gemma":[0.9733398,0.00007275433,0.000307507,0.008617229,0.00010468969,0.000014997017,0.0002999815,0.0000079591855,0.017235106],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9971324,0.00015614394,0.00058593496,0.00064301904,0.00088446966,0.00059800147],"domain_scores_gemma":[0.9983618,0.0005678101,0.00038531984,0.00041569312,0.00012377772,0.00014555245],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003708981,0.00045243464,0.00069756736,0.000033264674,0.00023573049,0.000040207637,0.0007217433,0.00034357578,0.0021963362],"category_scores_gemma":[0.00003368083,0.0002314896,0.0004940903,0.00012282385,0.00047499404,0.000030277433,0.00009301205,0.0008161915,0.000079288606],"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":[0.0008489743,0.00020576158,0.79825085,0.00033250422,0.0014684519,0.00012604607,0.007039946,0.013233666,0.00010983967,0.0008606415,0.024582079,0.15294121],"study_design_scores_gemma":[0.0014066702,0.0031761648,0.7299962,0.0003749627,0.00094488164,0.00005008002,0.003348498,0.011278585,0.00003058081,0.020536592,0.2265409,0.0023158751],"about_ca_topic_score_codex":0.568824,"about_ca_topic_score_gemma":0.6934565,"teacher_disagreement_score":0.35245383,"about_ca_system_score_codex":0.000049441398,"about_ca_system_score_gemma":0.0002180367,"threshold_uncertainty_score":0.9987158},"labels":[],"label_agreement":null},{"id":"W2980113723","doi":"10.1130/2018.2538(06)","title":"Quaternary glaciovolcanism in the Canadian Cascade volcanic arc—Paleoenvironmental implications","year":2019,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geology and Paleoclimatology Research","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":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Quaternary; Volcano; Geology; Cascade; Earth science; Geochemistry; Paleontology; Engineering","score_opus":0.027176478988229582,"score_gpt":0.22859372661949268,"score_spread":0.2014172476312631,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2980113723","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.028686335,0.0008214191,0.000010277623,0.0036863917,0.000104956336,0.0007247994,0.00024531447,0.00002125623,0.96569926],"genre_scores_gemma":[0.9261478,0.00040239253,0.00029563898,0.004338811,0.00006321689,0.000008068782,0.00038369728,0.000008125714,0.06835225],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99789244,0.00014377413,0.00040950844,0.000523309,0.00032858734,0.00070239033],"domain_scores_gemma":[0.9985882,0.00047621244,0.00021663746,0.0005013516,0.000024104698,0.00019350671],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00038955218,0.0003247014,0.00053437275,0.00007465977,0.00032370837,0.00001850223,0.0008929856,0.0007894106,0.0046105194],"category_scores_gemma":[0.000011986419,0.00022681421,0.00036816078,0.000038203452,0.002228005,0.000027515089,0.000056397956,0.0013081752,0.0009861231],"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":[0.00001658925,0.000010499027,0.9919092,0.000024817755,0.00008060583,0.000034629127,0.00053439155,0.00004885937,0.0000021577268,0.0025934866,0.0017576813,0.002987059],"study_design_scores_gemma":[0.00029306248,0.0004167847,0.875344,0.000027513604,0.00005034665,0.00019160731,0.00045359271,0.00038329186,0.0000018812923,0.015516144,0.10690018,0.00042159436],"about_ca_topic_score_codex":0.06387677,"about_ca_topic_score_gemma":0.24374989,"teacher_disagreement_score":0.8974615,"about_ca_system_score_codex":0.000017909364,"about_ca_system_score_gemma":0.0003017226,"threshold_uncertainty_score":0.99979174},"labels":[],"label_agreement":null},{"id":"W2980116679","doi":"10.1130/2018.2541(02)","title":"Taxonomy of Cretaceous–Paleogene coniferous woods and their distribution in fossil Lagerstätten of the high latitudes","year":2019,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological Studies and Exploration","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":"","keywords":"Paleogene; Geology; Swamp; Paleontology; Vegetation (pathology); Cretaceous; Ecology; Biology","score_opus":0.024906626059221525,"score_gpt":0.1802937601637353,"score_spread":0.15538713410451377,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2980116679","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.48949558,0.014733479,0.0013444999,0.0013384501,0.0003849254,0.0026719405,0.0017734331,0.00006100548,0.4881967],"genre_scores_gemma":[0.9948007,0.000968348,0.0005181105,0.00015006623,0.000030186577,0.0000033800507,0.000100263715,0.0000030116353,0.0034259313],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99878865,0.000051128638,0.00045635775,0.0002869112,0.00019820336,0.00021875973],"domain_scores_gemma":[0.99884933,0.00027441527,0.00054835196,0.00019818814,0.00008755943,0.0000421554],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017807192,0.00023820948,0.00071076927,0.000011416692,0.00008220474,0.000006569516,0.00022966896,0.00030930573,0.0004484297],"category_scores_gemma":[0.000025822468,0.00013034204,0.00028335754,0.000036128527,0.0014617903,0.000023800889,0.00010699735,0.0002587473,0.000004511755],"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":[0.00049530424,0.00012079918,0.45991638,0.00066022656,0.0008539479,0.0000043638656,0.0015365805,0.0031714882,0.00020519867,0.0053290776,0.0021303345,0.5255763],"study_design_scores_gemma":[0.0012128819,0.0024402903,0.7567215,0.00029778172,0.00015821298,0.0000066378525,0.0019011843,0.0013605624,0.00040669276,0.020941596,0.21374114,0.0008115005],"about_ca_topic_score_codex":0.00060330005,"about_ca_topic_score_gemma":0.00012897972,"teacher_disagreement_score":0.5247648,"about_ca_system_score_codex":0.000007317043,"about_ca_system_score_gemma":0.000034008743,"threshold_uncertainty_score":0.5386027},"labels":[],"label_agreement":null},{"id":"W2980139348","doi":"10.1130/2018.2541(12)","title":"Detrital zircon U-Pb and Lu-Hf analysis of Paleozoic sedimentary rocks from the Pearya terrane and Ellesmerian Fold Belt (northern Ellesmere Island): A comparison with Circum-Arctic datasets and their implications on terrane tectonics","year":2019,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","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":"Zircon; Geology; Terrane; Provenance; Devonian; Ordovician; Paleozoic; Laurentia; Sedimentary rock; Carboniferous; Clastic rock; Geochemistry; Paleontology; Basement; Late Devonian extinction; Detritus; Structural basin; Tectonics","score_opus":0.014165784397262186,"score_gpt":0.1977631807990221,"score_spread":0.18359739640175993,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2980139348","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96196425,0.0061737625,0.0008205085,0.003059088,0.00003632989,0.0009777168,0.010869787,0.000057919642,0.016040642],"genre_scores_gemma":[0.9916957,0.00090877456,0.0005873982,0.001532328,0.000038995968,0.0000041556386,0.0046306555,0.000009122713,0.00059287436],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99784493,0.00008320841,0.0005743714,0.0008417006,0.00029281853,0.00036296094],"domain_scores_gemma":[0.99754274,0.0011073947,0.000560717,0.00052291685,0.00006753729,0.00019867733],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00015933959,0.0005145944,0.0013586404,0.00007103607,0.00025543306,0.000034347016,0.0003649087,0.00034506398,0.0013564217],"category_scores_gemma":[0.00001723443,0.00027797528,0.0004018233,0.0001403168,0.0017478872,0.000041452175,0.00015642053,0.0006094878,0.000004846311],"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":[0.0004599146,0.00015399857,0.8823982,0.00012736741,0.008127229,0.0000064006567,0.0019425218,0.0006295725,0.0008261221,0.00006942148,0.00070885546,0.104550436],"study_design_scores_gemma":[0.0027518994,0.0054317834,0.927017,0.00039585956,0.010378566,0.00005085063,0.0061399536,0.010905988,0.0002960512,0.012976785,0.02137719,0.0022781035],"about_ca_topic_score_codex":0.007641329,"about_ca_topic_score_gemma":0.006505102,"teacher_disagreement_score":0.10227233,"about_ca_system_score_codex":0.000007149382,"about_ca_system_score_gemma":0.00003368176,"threshold_uncertainty_score":0.9999672},"labels":[],"label_agreement":null},{"id":"W2980164759","doi":"10.1130/2018.2541(05)","title":"Defining tectonic boundaries using detrital zircon signatures of Precambrian metasediments from Svalbard’s Southwestern Caledonian Basement Province","year":2019,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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 Ottawa","funders":"","keywords":"Geology; Zircon; Precambrian; Provenance; Basement; Geochemistry; Tectonics; Baltic Shield; Paleozoic; Arctic; Paleontology; Oceanography; Archaeology; Geography","score_opus":0.013661216118993935,"score_gpt":0.19824187685922154,"score_spread":0.1845806607402276,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2980164759","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.65947205,0.012745937,0.001723384,0.00033305242,0.0005185264,0.0019463267,0.007315809,0.0002550756,0.31568986],"genre_scores_gemma":[0.94794726,0.00008642792,0.029152669,0.000979246,0.00015129156,0.0000029739572,0.0014486116,0.00002288652,0.020208605],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.996748,0.000090387446,0.0008922062,0.0008748807,0.0008098528,0.00058471685],"domain_scores_gemma":[0.9977048,0.00054529065,0.00096396817,0.00042267237,0.00014311941,0.00022013395],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00023969999,0.00060474954,0.0015060569,0.000052260853,0.00022169632,0.00006181796,0.00057703594,0.00064875494,0.009952832],"category_scores_gemma":[0.0000591465,0.00043387036,0.0011771253,0.00006158694,0.002108065,0.000058208047,0.00020221328,0.00069493154,0.00014826642],"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":[0.0028260115,0.0009651683,0.52232426,0.0023943104,0.020700596,0.0002652391,0.0031900094,0.0124295065,0.068409994,0.005877292,0.0030355426,0.35758206],"study_design_scores_gemma":[0.012821215,0.020964405,0.2239241,0.0047165914,0.019050753,0.00007383052,0.003054728,0.0669913,0.051459536,0.21265829,0.36626235,0.018022908],"about_ca_topic_score_codex":0.008855059,"about_ca_topic_score_gemma":0.00040265443,"teacher_disagreement_score":0.3632268,"about_ca_system_score_codex":0.00002451919,"about_ca_system_score_gemma":0.00029093862,"threshold_uncertainty_score":0.9998113},"labels":[],"label_agreement":null},{"id":"W2980165038","doi":"10.1130/2018.2541(25)","title":"Age, geochemistry, and significance of Devonian felsic magmatism in the North Slope subterrane, Yukon, Canadian Arctic","year":2019,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":true,"ca_institutions":"McGill University; Yukon University","funders":"","keywords":"Geology; Felsic; Pluton; Terrane; Zircon; Geochemistry; Devonian; Arctic; Igneous rock; Continental crust; Magmatism; Crust; Mafic; Paleontology; Oceanography","score_opus":0.014766627654572088,"score_gpt":0.18148557848708274,"score_spread":0.16671895083251065,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2980165038","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.22545597,0.0015860145,0.00002271688,0.001542302,0.000051581148,0.0006494686,0.00041872438,0.000023586837,0.77024966],"genre_scores_gemma":[0.9811696,0.00037846767,0.0009223116,0.0018779333,0.00004514229,0.0000033539377,0.00029272458,0.0000053755525,0.0153051],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99787056,0.00006210245,0.000581657,0.0005603972,0.00040588234,0.0005194179],"domain_scores_gemma":[0.9984939,0.00042533013,0.00038736913,0.0003723505,0.00009563088,0.00022542574],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00023445406,0.00038600067,0.0008820214,0.000046800746,0.00009819817,0.000021300802,0.0006218221,0.0003923024,0.0062157298],"category_scores_gemma":[0.00004947211,0.00024182544,0.00040736518,0.00009381387,0.0017024387,0.000022617438,0.000056483,0.00067814364,0.000045761088],"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":[0.00014817379,0.00010046468,0.74057776,0.0013367338,0.00066256337,0.00023631967,0.0020815264,0.00064002816,0.00017357699,0.0027927458,0.0034647933,0.24778531],"study_design_scores_gemma":[0.0004668255,0.0005998809,0.87565917,0.00018847111,0.00022687668,0.000034484023,0.00048429135,0.0010744851,0.00003378583,0.07581894,0.044443306,0.0009695162],"about_ca_topic_score_codex":0.1311949,"about_ca_topic_score_gemma":0.11204547,"teacher_disagreement_score":0.75571364,"about_ca_system_score_codex":0.000013489543,"about_ca_system_score_gemma":0.00012765714,"threshold_uncertainty_score":0.99469274},"labels":[],"label_agreement":null},{"id":"W2980212797","doi":"10.1130/2019.2541(21)","title":"Evidence for the sinistral Porcupine shear zone in North Yukon (Canadian Arctic) and geotectonic implications","year":2019,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":"Yukon University","funders":"","keywords":"Sinistral and dextral; Geology; Paleozoic; Shear zone; Terrane; Paleontology; Arctic; Outcrop; Devonian; Shear (geology); Tectonics; Oceanography","score_opus":0.04529319446775905,"score_gpt":0.22577040353948025,"score_spread":0.1804772090717212,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2980212797","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.27684334,0.03406809,0.0037276878,0.092320606,0.0005066824,0.009083099,0.003876791,0.0003075935,0.57926613],"genre_scores_gemma":[0.97266847,0.0016045388,0.0019106887,0.002793311,0.00008583224,0.000010449816,0.00021751446,0.000006252179,0.02070294],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9982635,0.0000258366,0.00043673263,0.00056151155,0.00019932016,0.0005131133],"domain_scores_gemma":[0.9978252,0.0012575676,0.00023677378,0.0003371369,0.000110356596,0.00023297171],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00021487862,0.0003013329,0.0005978996,0.000040647992,0.0001982569,0.000026305042,0.00042380887,0.0003176426,0.0033731745],"category_scores_gemma":[0.00010593996,0.0001826537,0.00047559725,0.000076825585,0.0012030132,0.00003099187,0.000057763118,0.0005229444,0.00005459341],"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":[0.00029310165,0.000056636636,0.41938657,0.00042828498,0.00076543074,0.000012444766,0.00042813944,0.0045573167,0.00005227689,0.0084244935,0.0019934436,0.56360185],"study_design_scores_gemma":[0.00031728848,0.0008107243,0.8952189,0.00010040654,0.000247787,0.000015783962,0.000114148075,0.005811786,0.0000037066993,0.034544714,0.062238462,0.0005762845],"about_ca_topic_score_codex":0.06100475,"about_ca_topic_score_gemma":0.06313423,"teacher_disagreement_score":0.69582516,"about_ca_system_score_codex":0.000019263987,"about_ca_system_score_gemma":0.00014423086,"threshold_uncertainty_score":0.99753785},"labels":[],"label_agreement":null},{"id":"W2980213290","doi":"10.1130/2018.2541(17)","title":"Aeromagnetic high-resolution survey over the Vendom Fiord region, Ellesmere Island, Canadian High Arctic","year":2019,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological Studies and Exploration","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; Magnetic anomaly; Lineament; Aeromagnetic survey; Fjord; Fault (geology); Arctic; Structural basin; Basement; Seismology; Paleontology; Tectonics; Geomorphology; Oceanography; Geography","score_opus":0.023713351664956826,"score_gpt":0.18476932721164133,"score_spread":0.1610559755466845,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2980213290","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.13228524,0.008259681,0.00090245483,0.019794973,0.0036065036,0.0052831606,0.0058738296,0.00030381535,0.82369035],"genre_scores_gemma":[0.899573,0.0018113182,0.00031798487,0.005003481,0.00027282577,0.000006229815,0.0022754536,0.000014515917,0.090725146],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9977302,0.00015717636,0.0004759782,0.0005799782,0.00042828498,0.0006283888],"domain_scores_gemma":[0.99817187,0.0006213974,0.00042626492,0.0004188243,0.00015386268,0.00020780413],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003130361,0.00042445702,0.0007047315,0.000031025935,0.0004900184,0.000037789363,0.00046846815,0.00054939854,0.010384248],"category_scores_gemma":[0.00006841463,0.0002580975,0.00039719042,0.000058070542,0.0012013762,0.000034891902,0.000078036006,0.00064391585,0.00043815596],"study_design_candidate":"not_applicable","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":[0.00078637013,0.00008481953,0.2367944,0.00028513224,0.0015957032,0.00010108074,0.0014557468,0.00920207,0.0000038985586,0.014006165,0.4974508,0.23823382],"study_design_scores_gemma":[0.00042322837,0.001124486,0.5922521,0.00005079949,0.000102181955,0.000009227916,0.00015062414,0.0007753574,3.383596e-7,0.0097587705,0.39482942,0.00052347657],"about_ca_topic_score_codex":0.58708423,"about_ca_topic_score_gemma":0.35030648,"teacher_disagreement_score":0.7672878,"about_ca_system_score_codex":0.00003597984,"about_ca_system_score_gemma":0.00013380901,"threshold_uncertainty_score":0.9999871},"labels":[],"label_agreement":null},{"id":"W2980218589","doi":"10.1130/2018.2541(14)","title":"Triassic history of the Tanquary High in NE Sverdrup Basin, Canadian Arctic Archipelago","year":2019,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological Studies and Exploration","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":"Paleontology; Geology; Isopach map; Sverdrup; Sequence (biology); Early Triassic; Facies; Tectonics; Unconformity; Structural basin; Diachronous; Permian","score_opus":0.02401047014719728,"score_gpt":0.17526766149066367,"score_spread":0.15125719134346638,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2980218589","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.020912305,0.0027184018,0.000027712471,0.0022547022,0.0010157324,0.0009118161,0.00017598424,0.000030838648,0.9719525],"genre_scores_gemma":[0.8844556,0.00058296416,0.00061641465,0.0036805186,0.000113521986,0.0000032322412,0.00011027031,0.000008923293,0.110428534],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99811053,0.00009464336,0.0005515268,0.0004166414,0.00037853225,0.00044811284],"domain_scores_gemma":[0.99861825,0.0003378728,0.00047957222,0.00033861573,0.00008013326,0.0001455467],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00025320475,0.00030865922,0.0007983344,0.00004622271,0.000089649286,0.000005252176,0.00047108423,0.00042037762,0.0037711053],"category_scores_gemma":[0.0000581077,0.00019210055,0.0005345384,0.00004532453,0.0014441583,0.000027264548,0.000076286364,0.00064926274,0.00009230635],"study_design_candidate":"design_other","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":[0.0008068037,0.00014995824,0.20839018,0.00083613663,0.0009262449,0.00005856293,0.009504706,0.0036661462,0.000048347123,0.020434944,0.08573674,0.6694412],"study_design_scores_gemma":[0.0007307963,0.0012837517,0.38563296,0.00019883925,0.00010873623,0.0000057240327,0.0008400449,0.00068690407,0.0000027386293,0.040423803,0.5694153,0.000670447],"about_ca_topic_score_codex":0.26349998,"about_ca_topic_score_gemma":0.050590456,"teacher_disagreement_score":0.86354333,"about_ca_system_score_codex":0.00012709032,"about_ca_system_score_gemma":0.00042441895,"threshold_uncertainty_score":0.9971396},"labels":[],"label_agreement":null},{"id":"W2980246686","doi":"10.1130/2018.2541(23)","title":"Pre-Mississippian stratigraphy and provenance of the North Slope of Arctic Alaska II: Basinal rocks of the northeastern Brooks Range and their significance in circum-Arctic evolution","year":2019,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological Studies and Exploration","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":"Yukon University","funders":"","keywords":"Geology; Geochronology; Siliciclastic; Paleontology; Zircon; Ordovician; Devonian; Diamictite; Dolostone; Arctic; Provenance; Geochemistry; Sedimentary rock; Carbonate rock; Clastic rock; Structural basin; Sedimentary depositional environment; Oceanography","score_opus":0.013114122981466594,"score_gpt":0.17293828409602435,"score_spread":0.15982416111455777,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2980246686","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9680662,0.0028972663,0.00015517038,0.00040229698,0.000089879984,0.0013026951,0.00018152242,0.000009291318,0.026895681],"genre_scores_gemma":[0.9972007,0.00036800126,0.00013666152,0.000117309726,0.00001982346,0.0000042295806,0.000008129789,0.0000041786793,0.0021409523],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983667,0.0000940489,0.0005844262,0.00038409306,0.00031870918,0.0002520079],"domain_scores_gemma":[0.9984132,0.00021150187,0.00090047176,0.00029218968,0.00012789157,0.000054747667],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018074753,0.00028478875,0.00069689867,0.000021624654,0.00015524798,0.000006262568,0.00031896104,0.0002220391,0.00007923951],"category_scores_gemma":[0.000035523924,0.00014448834,0.00031939807,0.00007987391,0.0020761238,0.00004050943,0.00013090449,0.00037637103,5.4268213e-7],"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":[0.00012059364,0.00003198511,0.9747771,0.00043220117,0.0000919465,2.1220713e-7,0.001351448,0.000518127,0.0000527259,0.00024306207,0.000013101276,0.022367466],"study_design_scores_gemma":[0.00028911192,0.0008050869,0.9904119,0.00029668843,0.000048896156,0.000002693244,0.0005226168,0.0006369495,0.000023290344,0.0062099686,0.00058276753,0.0001700649],"about_ca_topic_score_codex":0.0030276615,"about_ca_topic_score_gemma":0.00186545,"teacher_disagreement_score":0.029134518,"about_ca_system_score_codex":0.000008667032,"about_ca_system_score_gemma":0.00007502763,"threshold_uncertainty_score":0.7649565},"labels":[],"label_agreement":null},{"id":"W2980252763","doi":"10.1130/2018.2541(11)","title":"Episodic tectonics in the Phanerozoic succession of the Canadian High Arctic and the “10-million-year flood”","year":2019,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological Studies and Exploration","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":true,"ca_institutions":"University of Calgary; Geological Survey of Canada","funders":"","keywords":"Geology; Tectonics; Phanerozoic; Paleontology; Tectonic subsidence; Plate tectonics; Unconformity; Tectonic phase; Structural basin; Thermal subsidence; Lithosphere; Seismology; Rift; Cenozoic","score_opus":0.015288584066411027,"score_gpt":0.18559886313498364,"score_spread":0.1703102790685726,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2980252763","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.1121586,0.006608871,0.000034979275,0.02929595,0.00069320435,0.0033963537,0.00036736246,0.00004150052,0.84740317],"genre_scores_gemma":[0.98571146,0.0011333596,0.00014019462,0.0022908896,0.000058716203,0.0000042671873,0.000055755678,0.0000039803385,0.010601406],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99843514,0.00015784492,0.0003728213,0.00029877428,0.00040714574,0.00032826516],"domain_scores_gemma":[0.99851894,0.0006929642,0.0003427954,0.00031210372,0.00006925541,0.00006393996],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00054621784,0.00023878195,0.0005094632,0.000020880929,0.00040354233,0.000024954401,0.0005564034,0.00031718222,0.0017222617],"category_scores_gemma":[0.00007628448,0.00009224871,0.00029492727,0.000068806636,0.0023916538,0.000021684818,0.00009268363,0.00057603634,0.00004039702],"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":[0.0015443746,0.00015366907,0.4205541,0.0010355086,0.0013175776,0.00003274591,0.016834164,0.007208191,0.000018703502,0.14108913,0.023438724,0.3867731],"study_design_scores_gemma":[0.0027680947,0.0014750621,0.5111451,0.00036158192,0.00033539586,0.000023768906,0.0038781248,0.0027944883,0.00000848336,0.15275176,0.3235067,0.00095140736],"about_ca_topic_score_codex":0.16193354,"about_ca_topic_score_gemma":0.0536055,"teacher_disagreement_score":0.87355286,"about_ca_system_score_codex":0.000014715364,"about_ca_system_score_gemma":0.000093104965,"threshold_uncertainty_score":0.9991903},"labels":[],"label_agreement":null},{"id":"W3017335944","doi":"10.1130/2020.2544(02)","title":"The Central Iapetus magmatic province: An updated review and link with the ca. 580 Ma Gaskiers glaciation","year":2020,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","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":"Carleton University","funders":"","keywords":"Glacial period; Geology; Link (geometry); Physical geography; Paleontology; Geography; Computer science; Computer network","score_opus":0.008491148360028277,"score_gpt":0.17896719399568953,"score_spread":0.17047604563566124,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3017335944","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.007295135,0.04321454,0.00048247955,0.13464932,0.00012748108,0.0038698297,0.00052232924,0.0003512946,0.8094876],"genre_scores_gemma":[0.5176552,0.058786258,0.010701322,0.13549767,0.0012714225,0.000059399707,0.0059847287,0.00007302958,0.26997098],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9981081,0.00010929038,0.00041945174,0.00050311786,0.00042628153,0.00043376713],"domain_scores_gemma":[0.9986176,0.0002556657,0.00048399452,0.00029526785,0.00009575899,0.00025169566],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00023782531,0.00036418557,0.0006989232,0.000007669252,0.00039462448,0.00005079838,0.00047435903,0.00022565933,0.0037752322],"category_scores_gemma":[0.00003311941,0.0001507913,0.00032918883,0.00006361365,0.0019343816,0.000036384226,0.00007554459,0.00063276844,0.000055993725],"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":[0.0006106036,0.00007854393,0.018024156,0.0018281639,0.0028247621,0.000075846474,0.0009971006,0.00036075854,0.00007072319,0.0075033475,0.07170029,0.8959257],"study_design_scores_gemma":[0.00055759825,0.0026859078,0.033736765,0.00030758526,0.0025785733,0.000048455244,0.000680505,0.007965828,0.000016698004,0.05377307,0.8963183,0.0013306946],"about_ca_topic_score_codex":0.00048143638,"about_ca_topic_score_gemma":0.00022035155,"teacher_disagreement_score":0.894595,"about_ca_system_score_codex":0.000007295833,"about_ca_system_score_gemma":0.00006149033,"threshold_uncertainty_score":0.99713546},"labels":[],"label_agreement":null},{"id":"W3025717159","doi":"10.1130/2020.2546(03)","title":"Origin and evolution of the Grenvillian Oaxacan Complex, southern Mexico: Hf isotopic and U-Pb geochronologic constraints","year":2020,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","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":"Zircon; Geology; Geochemistry; Granulite; Metamorphism; Craton; Geochronology; Gneiss; Igneous rock; Crust; Protolith; Continental arc; Laurentia; Petrology; Metamorphic rock; Facies; Ordovician; Geomorphology; Volcanic rock; Paleontology; Tectonics","score_opus":0.02092103858403497,"score_gpt":0.18795081995679533,"score_spread":0.16702978137276037,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3025717159","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.2805594,0.0047292085,0.0009155084,0.008660374,0.00015315598,0.001267259,0.0017072203,0.00017767005,0.7018302],"genre_scores_gemma":[0.98997986,0.00021747709,0.0020421047,0.0011830911,0.000059100727,0.0000015289679,0.0000718803,0.0000045916795,0.0064403554],"study_design_codex":"observational","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9982792,0.00006627778,0.0004767987,0.000552429,0.0003123686,0.00031289013],"domain_scores_gemma":[0.9988241,0.00021349228,0.00049334345,0.00022316433,0.000063945525,0.00018192423],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00011259618,0.00035335746,0.00081864535,0.00002030563,0.00016708048,0.000013630376,0.00035081146,0.0004115535,0.0056316894],"category_scores_gemma":[0.00004198898,0.00020339726,0.00044573648,0.000051436997,0.005894962,0.000016141401,0.00018353609,0.0005127744,0.000030768097],"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":[0.00019195372,0.00009608068,0.6596575,0.0005784072,0.0014880536,0.000021088035,0.0012713597,0.00020099405,0.0019021715,0.024669176,0.0025050323,0.3074182],"study_design_scores_gemma":[0.0011219197,0.0019806586,0.39480993,0.00018885611,0.0007729587,0.000055884695,0.0020069852,0.0053260694,0.00015026964,0.5273728,0.064795114,0.0014185779],"about_ca_topic_score_codex":0.0016189116,"about_ca_topic_score_gemma":0.00013981966,"teacher_disagreement_score":0.7094205,"about_ca_system_score_codex":0.000008891426,"about_ca_system_score_gemma":0.000041517804,"threshold_uncertainty_score":0.99681044},"labels":[],"label_agreement":null},{"id":"W3034277418","doi":"10.1130/2020.2548(02)","title":"Pliocene–Pleistocene landscape evolution and watershed reorganization east of the central Andes in Argentine Patagonia","year":2020,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geology and Paleoclimatology Research","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":"University of Northern British Columbia; University of Lethbridge; Simon Fraser University; Douglas College","funders":"","keywords":"Geology; Pleistocene; Paleontology; Early Pleistocene; Geomorphology; Structural basin","score_opus":0.01633159554438891,"score_gpt":0.19439792388326876,"score_spread":0.17806632833887986,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3034277418","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8191274,0.0030454488,0.00024867253,0.0032275124,0.00026503165,0.0011530917,0.00040868332,0.0000729044,0.1724513],"genre_scores_gemma":[0.99558514,0.00022982509,0.0003630031,0.00021181279,0.000037702222,8.776294e-7,0.00021312007,0.000004566057,0.0033539322],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987032,0.000088560635,0.00035229177,0.00033407332,0.00021201835,0.00030988973],"domain_scores_gemma":[0.99932784,0.00010024024,0.0002630332,0.00016091352,0.000060857194,0.00008710191],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00014861116,0.00019751131,0.00047751784,0.000032295222,0.00010779341,0.0000057533343,0.0002413893,0.00039130595,0.0011954027],"category_scores_gemma":[0.000039066734,0.00012931877,0.00015140517,0.000063235224,0.0012919098,0.000021726128,0.000088666646,0.00042145955,0.000012748862],"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":[0.000103228274,0.000008916038,0.9973563,0.00008280273,0.000047909587,0.0000033432,0.00028484137,0.000041016105,0.000027471902,0.00068125455,0.00020405621,0.0011588417],"study_design_scores_gemma":[0.00039608628,0.00027711783,0.9917684,0.000043238535,0.000040097617,0.000016627151,0.00016499321,0.0012052717,0.00004792595,0.004431894,0.0014369893,0.00017135206],"about_ca_topic_score_codex":0.00017403907,"about_ca_topic_score_gemma":0.0001256528,"teacher_disagreement_score":0.1764578,"about_ca_system_score_codex":0.0000030287229,"about_ca_system_score_gemma":0.000061669874,"threshold_uncertainty_score":0.99971765},"labels":[],"label_agreement":null},{"id":"W3034478244","doi":"10.1130/2020.2548(05)","title":"Deglacial landforms and Holocene vegetation trajectories in the northern interior cedar-hemlock forests of British Columbia","year":2020,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geology and Paleoclimatology Research","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":"Royal British Columbia Museum; University of Victoria; University of Northern British Columbia","funders":"","keywords":"Tsuga; Geology; Western Hemlock; Holocene; Dominance (genetics); Terrace (agriculture); Physical geography; Ecology; Forestry; Geography; Paleontology; Archaeology","score_opus":0.01747617434350468,"score_gpt":0.2142918367020355,"score_spread":0.19681566235853082,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3034478244","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9067345,0.00094685133,0.000020125992,0.00022270996,0.000057860638,0.00036197685,0.00010405664,0.00001859859,0.09153331],"genre_scores_gemma":[0.99515355,0.0002322864,0.00034066872,0.00040797255,0.00004602178,0.0000039207844,0.000107412765,0.0000044229882,0.0037037288],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99869424,0.00008192613,0.00038528506,0.00031929268,0.00024814522,0.0002711007],"domain_scores_gemma":[0.99911475,0.00037269376,0.00025135826,0.00012766666,0.00006704924,0.00006645279],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023468868,0.0001563446,0.0005735401,0.000017028267,0.00010231574,0.00002455624,0.00030428555,0.00043081475,0.00033313726],"category_scores_gemma":[0.000042042113,0.00014192196,0.0001964458,0.000039492686,0.002112416,0.0000281238,0.000047024867,0.0005744221,0.000012350588],"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":[0.0000578356,0.0000064536935,0.98225576,0.00011126065,0.0000537372,0.00002542323,0.00086627714,0.000006176406,8.6517804e-7,0.00003805183,0.00019897228,0.016379206],"study_design_scores_gemma":[0.00036508575,0.00080398185,0.9870947,0.00007233503,0.000035500037,0.000074712705,0.00055929314,0.00016296556,0.000001882727,0.00908213,0.0015605035,0.00018690081],"about_ca_topic_score_codex":0.0045588585,"about_ca_topic_score_gemma":0.08294189,"teacher_disagreement_score":0.08841906,"about_ca_system_score_codex":0.0000017442185,"about_ca_system_score_gemma":0.000059920152,"threshold_uncertainty_score":0.93379205},"labels":[],"label_agreement":null},{"id":"W3035733546","doi":"10.1130/2020.2545(05)","title":"Late Devonian lonestones, diamictites, and coeval black shales from the Appalachian Basin: Discerning relationships and implications for Late Devonian Appalachian history and glacially driven seafloor anoxia","year":2020,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":"University of Calgary","funders":"","keywords":"Devonian; Geology; Late Devonian extinction; Paleontology; Seafloor spreading; Structural basin; Geochemistry; Carboniferous","score_opus":0.04137732036137927,"score_gpt":0.2276573783736684,"score_spread":0.18628005801228914,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3035733546","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.73320246,0.024479356,0.0018461684,0.047514863,0.00034620127,0.0043484755,0.0035062234,0.00036016598,0.18439612],"genre_scores_gemma":[0.96846867,0.0022901506,0.0095503805,0.0024419625,0.00021899526,0.000024580373,0.0012917678,0.000032232347,0.01568129],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99787533,0.0002290283,0.0004513314,0.0008024274,0.00018090522,0.00046095753],"domain_scores_gemma":[0.99705356,0.0018968367,0.00037524122,0.00029289734,0.000077196855,0.00030425194],"candidate_categories":["metaepi_narrow","sts"],"consensus_categories":[],"category_scores_codex":[0.00036432047,0.00042344688,0.0007258813,0.000041153766,0.00084427174,0.000042238644,0.0003335795,0.00066968956,0.00028582301],"category_scores_gemma":[0.00009665694,0.00031986868,0.00020714609,0.000034060824,0.005041891,0.000060576636,0.00014912378,0.0010720162,0.000025090663],"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":[0.00009869286,0.0000077117875,0.98966074,0.00008119169,0.00021422688,0.000004244984,0.001857118,0.000023650193,0.0000081324715,0.0029948556,0.00069652987,0.004352922],"study_design_scores_gemma":[0.00045161234,0.00029115134,0.9223518,0.000054169475,0.0001904543,0.000025991529,0.00030052115,0.0025791735,3.832612e-7,0.015731877,0.05762105,0.00040181982],"about_ca_topic_score_codex":0.00044352404,"about_ca_topic_score_gemma":0.001571793,"teacher_disagreement_score":0.23526621,"about_ca_system_score_codex":0.000010498409,"about_ca_system_score_gemma":0.00015524907,"threshold_uncertainty_score":0.9999253},"labels":[],"label_agreement":null},{"id":"W3037992015","doi":"10.1130/2020.2545(10)","title":"Ammonoids from the Tully Formation and Harrell Shale in Pennsylvania: Markers of sea-level highstands in the Middle to Late Devonian transition, Appalachian foreland basin, eastern North America","year":2020,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Paleontology and Stratigraphy of Fossils","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":"Devonian; Geology; Paleontology; Ordovician; Foreland basin; Honor; Archaeology; West virginia; Pennsylvanian; Stratigraphy; Structural basin; Geography","score_opus":0.028670780819966,"score_gpt":0.18848071089455012,"score_spread":0.15980993007458413,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3037992015","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7043047,0.002766205,0.0026115642,0.0053890655,0.00009274435,0.0015549737,0.0029167407,0.000039785722,0.28032425],"genre_scores_gemma":[0.9943601,0.0002578905,0.0023963116,0.002296094,0.000041187108,0.0000068412255,0.00022917383,0.000003458699,0.0004089683],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983472,0.00012420198,0.0005497053,0.00037425052,0.0003045746,0.0003000675],"domain_scores_gemma":[0.99891305,0.0004337168,0.00030419146,0.0002030173,0.00003740049,0.000108644286],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002335044,0.00030121987,0.00060236815,0.000041625757,0.00014221609,0.000022340622,0.00041991545,0.00027539275,0.00014283037],"category_scores_gemma":[0.000014163303,0.00018641789,0.00025728162,0.00008965204,0.000994102,0.00006504292,0.000011639483,0.0005727259,0.0000064161954],"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":[0.0010265104,0.000042743923,0.67371345,0.00014751732,0.00023398017,0.000042963013,0.033724923,0.0002353225,0.000007271592,0.00016116613,0.0012666722,0.28939748],"study_design_scores_gemma":[0.0004624023,0.0006853112,0.98648274,0.00009126627,0.000054418415,0.0000052135256,0.0022693567,0.0024982805,0.0000015287568,0.002968652,0.004229299,0.00025150648],"about_ca_topic_score_codex":0.0041075293,"about_ca_topic_score_gemma":0.009323108,"teacher_disagreement_score":0.31276932,"about_ca_system_score_codex":0.000005370071,"about_ca_system_score_gemma":0.000045165267,"threshold_uncertainty_score":0.7601901},"labels":[],"label_agreement":null},{"id":"W3041661417","doi":"10.1130/fld058","title":"Architecture and Evolution of the Crust during Continental Arc Magmatism: A Transect through the Coast Mountains Batholith, British Columbia","year":2020,"lang":"en","type":"book","venue":"Geological Society of America eBooks","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":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Batholith; Transect; Geology; Continental margin; Continental crust; Magmatism; Oceanography; Crust; Intertidal zone; Paleontology; Archaeology; Geography; Tectonics","score_opus":0.006544310635379377,"score_gpt":0.16425842462024828,"score_spread":0.1577141139848689,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3041661417","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8801811,0.0035086186,0.0005497421,0.002984836,0.000105120576,0.0010686702,0.0018071433,0.00009703672,0.10969778],"genre_scores_gemma":[0.9718807,0.00025971062,0.0009900936,0.0012530792,0.00012731597,0.0000062693694,0.000094950265,0.000006660736,0.025381256],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978817,0.00017645984,0.00053227507,0.0005123826,0.00049650716,0.00040067063],"domain_scores_gemma":[0.9988087,0.00031230753,0.0004500355,0.00024363151,0.00007213831,0.000113230315],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001206402,0.0002751942,0.0008090344,0.000006931457,0.00039842035,0.000065000764,0.0005646107,0.00033430153,0.0020782123],"category_scores_gemma":[0.000061378894,0.00018533767,0.0008569061,0.00013333219,0.0035123162,0.000026694444,0.0001600324,0.0008779227,0.000004831483],"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":[0.0006474416,0.000382692,0.7294349,0.0031813402,0.0033764222,0.00012560014,0.0139086135,0.003033371,0.0032555205,0.0005622103,0.07237194,0.16971995],"study_design_scores_gemma":[0.0009062557,0.00060637825,0.86887765,0.0002863914,0.00060642895,0.00021420281,0.0020888497,0.0011494472,0.0000659501,0.09627762,0.028181756,0.000739046],"about_ca_topic_score_codex":0.054118734,"about_ca_topic_score_gemma":0.018161185,"teacher_disagreement_score":0.1689809,"about_ca_system_score_codex":0.000014261512,"about_ca_system_score_gemma":0.00007651922,"threshold_uncertainty_score":0.9997548},"labels":[],"label_agreement":null},{"id":"W3082459521","doi":"10.1130/2018.2536(09)","title":"Evidence for a large middle Holocene flood event in the Pacific southwestern United States (Lake Elsinore, California)","year":2019,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geology and Paleoclimatology Research","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":"University of Saskatchewan","funders":"","keywords":"Silt; Geology; Flood myth; Storm; Hydrology (agriculture); Holocene; Sediment; Oceanography; Physical geography; Archaeology; Geography; Geomorphology","score_opus":0.07173712751261652,"score_gpt":0.2671835757797323,"score_spread":0.19544644826711577,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3082459521","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5980824,0.016442524,0.0027918497,0.010052091,0.0008483739,0.009169396,0.011439916,0.0003107501,0.35086268],"genre_scores_gemma":[0.94095,0.001517666,0.0009012935,0.0034516763,0.00009896877,0.000029236495,0.0029666084,0.000016103539,0.05006845],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9972627,0.00023945178,0.0005728952,0.0006331768,0.00044011816,0.0008516362],"domain_scores_gemma":[0.9963317,0.0025696033,0.00037235976,0.00046895203,0.00014526292,0.00011213274],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010857942,0.0004039595,0.00078423606,0.00009191714,0.0002347768,0.000026414216,0.0007965254,0.00074308855,0.001619725],"category_scores_gemma":[0.000092234455,0.00025771174,0.00054995477,0.00008362372,0.0011823733,0.00003444362,0.00008600446,0.00095021375,0.00035812287],"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":[0.00026174652,0.00004202297,0.99380404,0.00024050934,0.00014553608,0.000023636072,0.001433969,0.00022788926,2.996329e-7,0.00034680674,0.0013456248,0.0021279508],"study_design_scores_gemma":[0.0038118956,0.005798297,0.41787508,0.0013022209,0.0004973472,0.00020578771,0.010406464,0.015790964,0.000010495852,0.04108707,0.5009378,0.002276558],"about_ca_topic_score_codex":0.00020972682,"about_ca_topic_score_gemma":0.00072932587,"teacher_disagreement_score":0.5759289,"about_ca_system_score_codex":0.0000037580226,"about_ca_system_score_gemma":0.00012454185,"threshold_uncertainty_score":0.9999875},"labels":[],"label_agreement":null},{"id":"W3089191232","doi":"10.1130/2020.2548(07)","title":"Glacier development in continental climate regions of central Asia","year":2020,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Glacier; Moraine; Glacial period; Geology; Physical geography; Glacier mass balance; Climate change; Central asia; Last Glacial Maximum; Climatology; Arid; Mountain range (options); Geography; Geomorphology; Paleontology; Oceanography","score_opus":0.02887683886640377,"score_gpt":0.22809462292737767,"score_spread":0.1992177840609739,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3089191232","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.03796292,0.0008457624,0.00006989452,0.0010433919,0.00013245174,0.00053237996,0.00012823992,0.00004982136,0.95923513],"genre_scores_gemma":[0.9684664,0.00062614295,0.006252874,0.00086858455,0.000055000968,0.0000040603645,0.000431062,0.000009630242,0.023286253],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9978976,0.00007573103,0.00064399774,0.00045290997,0.00031284013,0.0006169234],"domain_scores_gemma":[0.9989411,0.0002724015,0.00036669895,0.00018295227,0.000057863264,0.00017895033],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00021389737,0.00029262542,0.0008658387,0.000049636506,0.00010301435,0.000004885843,0.0003852591,0.0005820436,0.0025623532],"category_scores_gemma":[0.000027130867,0.00023853357,0.00036307648,0.000043547174,0.0020587451,0.000020577028,0.00010772034,0.0007729707,0.00013507306],"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":[0.00016510721,0.000023637593,0.9885728,0.00013568418,0.00014119805,0.000049646547,0.00064379594,0.000023330673,0.0000073662854,0.003761651,0.00065507786,0.005820726],"study_design_scores_gemma":[0.0013065942,0.000975146,0.81155103,0.00023383973,0.000086965374,0.00007819482,0.0008183159,0.0006111706,0.00014117344,0.008900528,0.17441396,0.0008830851],"about_ca_topic_score_codex":0.00009199533,"about_ca_topic_score_gemma":0.0001439406,"teacher_disagreement_score":0.9359489,"about_ca_system_score_codex":0.0000042011025,"about_ca_system_score_gemma":0.00014490202,"threshold_uncertainty_score":0.9983494},"labels":[],"label_agreement":null},{"id":"W3092266201","doi":"10.1130/2020.2548(06)","title":"Climate of the Last Glacial Maximum on the western Olympic Peninsula based on insect paleoecology, palynology, and glacial geology","year":2020,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geology and Paleoclimatology Research","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":"Last Glacial Maximum; Glacial period; Geology; Macrofossil; Boreal; Paleoecology; Vegetation (pathology); Peninsula; Climate change; Physical geography; Ecology; Palynology; Geography; Pollen; Oceanography; Holocene; Paleontology; Archaeology","score_opus":0.027750277940715214,"score_gpt":0.22506364444633992,"score_spread":0.1973133665056247,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3092266201","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.3100531,0.00045667263,0.000025272202,0.020013526,0.0006834391,0.001615803,0.00035092488,0.00010841488,0.66669285],"genre_scores_gemma":[0.9834041,0.00022052752,0.00014877871,0.011874835,0.00014256928,0.000011880757,0.00008678333,0.000013739357,0.004096805],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.996792,0.0005956008,0.0006430976,0.00079183216,0.0004247803,0.000752686],"domain_scores_gemma":[0.9959624,0.0025595864,0.0006727874,0.000560463,0.00009142923,0.0001533656],"candidate_categories":["metaepi_narrow","sts","research_integrity","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005359806,0.0005414733,0.0011536669,0.00006683352,0.00052647083,0.000013184004,0.000967964,0.0013113096,0.0020242538],"category_scores_gemma":[0.00016603898,0.0003048397,0.00061596703,0.000072614544,0.009694412,0.0000161237,0.00028336304,0.0018223984,0.00019014672],"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":[0.0006633097,0.000034331668,0.9909059,0.00008081492,0.00017043068,0.000028910972,0.00021924691,0.00008235797,0.000005923014,0.0025500762,0.00073039654,0.004528294],"study_design_scores_gemma":[0.0014426954,0.0052865846,0.9503117,0.00010136764,0.00019291166,0.00008336881,0.00017709898,0.001465542,0.00004130298,0.012690945,0.027569365,0.00063710543],"about_ca_topic_score_codex":0.00007794604,"about_ca_topic_score_gemma":0.0005473414,"teacher_disagreement_score":0.673351,"about_ca_system_score_codex":0.0000046788173,"about_ca_system_score_gemma":0.00014849879,"threshold_uncertainty_score":0.9999852},"labels":[],"label_agreement":null},{"id":"W3093707810","doi":"10.1130/2017.0048(04)","title":"The Mesoproterozoic Belt Supergroup in Glacier and Waterton Lakes national parks, northwestern Montana and southwestern Alberta: Sedimentary facies and syndepositional deformation","year":2017,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological formations and processes","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 Saskatchewan","funders":"","keywords":"Geology; Facies; Supergroup; Sedimentary depositional environment; Sedimentary rock; Lithology; Structural basin; Paleontology; Glacier; Geochemistry","score_opus":0.0124126123809212,"score_gpt":0.19652554448816092,"score_spread":0.18411293210723972,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3093707810","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.90559846,0.0041377866,0.00007562553,0.0022673886,0.00010278813,0.00067709247,0.00046297192,0.000038972248,0.08663892],"genre_scores_gemma":[0.9846753,0.0018195611,0.00044612747,0.00089601724,0.000045277025,0.000011002772,0.0005161882,0.000004893993,0.011585646],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99869305,0.000031713782,0.00038682573,0.00030271843,0.00033140284,0.00025427935],"domain_scores_gemma":[0.9991113,0.0003267992,0.00026110513,0.00011452437,0.000071941715,0.00011431981],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021965196,0.0002717642,0.00034323442,0.000031399006,0.0006068713,0.00012919333,0.0001694901,0.00025547395,0.00012887044],"category_scores_gemma":[0.00001895795,0.00016181721,0.000087731314,0.0000103545935,0.0014030349,0.0002112356,0.00009332796,0.00028125875,0.0000067806263],"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":[0.00031217464,0.000045773675,0.7210316,0.0005749962,0.00047486403,0.000017090682,0.007898764,0.0001684981,0.000022799182,0.0046018003,0.00040747784,0.26444414],"study_design_scores_gemma":[0.0010100183,0.0009704889,0.865207,0.0002392796,0.00011017955,0.00023782412,0.0014527316,0.00475241,0.000012404201,0.055597976,0.06949586,0.0009138282],"about_ca_topic_score_codex":0.0032732585,"about_ca_topic_score_gemma":0.0034682069,"teacher_disagreement_score":0.2635303,"about_ca_system_score_codex":0.0000071229197,"about_ca_system_score_gemma":0.000032872707,"threshold_uncertainty_score":0.65987146},"labels":[],"label_agreement":null},{"id":"W3094008450","doi":"10.1130/2018.2530(10)","title":"Minimum age of the Mapleton, Tully, and Labrador Hollow moraines indicates correlation with the Port Huron Phase in central New York State","year":2018,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":"","keywords":"Moraine; Geology; Port (circuit theory); Geomorphology; Engineering; Mechanical engineering","score_opus":0.021835621148093835,"score_gpt":0.2238897908438838,"score_spread":0.20205416969578996,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3094008450","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.92043763,0.0013274566,0.000111199246,0.0027924434,0.00016286755,0.0009728252,0.0001391347,0.000029059462,0.0740274],"genre_scores_gemma":[0.9263446,0.00019377808,0.0006474131,0.0006609446,0.000064257874,0.0000023358218,0.00014643303,0.000007128243,0.07193311],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984459,0.00012156768,0.00035195102,0.0003558006,0.00030517325,0.0004195911],"domain_scores_gemma":[0.9987284,0.0004322627,0.00044334127,0.00024522012,0.000044310877,0.00010647932],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002972847,0.00025804722,0.0005188161,0.000034626108,0.00016618935,0.000011558059,0.00040598,0.00035138737,0.0011988502],"category_scores_gemma":[0.00002480167,0.0001293915,0.00016724323,0.00006327084,0.0050116763,0.00002317514,0.00007231511,0.0006276866,0.000015450145],"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":[0.00042545673,0.000029073593,0.982439,0.00006681975,0.00016725728,0.000021793798,0.0038546312,0.000103759514,0.000015070327,0.00014685854,0.004627232,0.008103093],"study_design_scores_gemma":[0.0023332804,0.0027193313,0.9396476,0.00018394049,0.00017158304,0.00009464039,0.001412121,0.0012281161,0.000044455686,0.014204524,0.037396394,0.00056398165],"about_ca_topic_score_codex":0.0008936833,"about_ca_topic_score_gemma":0.00071244646,"teacher_disagreement_score":0.042791322,"about_ca_system_score_codex":0.0000020922482,"about_ca_system_score_gemma":0.00013604791,"threshold_uncertainty_score":0.9997142},"labels":[],"label_agreement":null},{"id":"W3094766611","doi":"10.1130/2020.2548(12)","title":"A 3 m.y. record of volcanism and glaciation in northern British Columbia, Canada","year":2020,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geology and Paleoclimatology Research","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":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Glacial period; Pleistocene; Paleontology; Interglacial; Ice sheet; Volcano; Lava; Volcanism; Geomorphology; Tectonics","score_opus":0.012823621509896965,"score_gpt":0.1841819008123338,"score_spread":0.17135827930243683,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3094766611","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.47842252,0.0012800512,0.0000146806,0.0006644468,0.00011586984,0.00048479563,0.00027295284,0.000023866636,0.5187208],"genre_scores_gemma":[0.9588396,0.00056501693,0.0009475972,0.0010973,0.000037767426,0.0000023361363,0.00016077711,0.000006009529,0.038343593],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99867976,0.000061818464,0.0003968097,0.00035166182,0.00024281918,0.000267142],"domain_scores_gemma":[0.9991036,0.00030302253,0.00029419517,0.00011266818,0.00007373555,0.00011277856],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00013968509,0.00013676981,0.00062967924,0.000013053785,0.00007802478,0.0000117738555,0.00019256974,0.0003993512,0.0014763883],"category_scores_gemma":[0.000043129286,0.00017172062,0.00012332945,0.000029140943,0.0010272072,0.000014862471,0.000047875,0.00052640605,0.00000773426],"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":[0.000018578203,0.0000036721622,0.97014767,0.00006881631,0.000050215367,0.000038051403,0.00007867906,0.000004802323,5.9945415e-7,0.000022094258,0.000912257,0.02865459],"study_design_scores_gemma":[0.00035302519,0.0004890465,0.9629791,0.00007075955,0.000030216737,0.000036659992,0.00020610895,0.00033390167,8.419157e-7,0.009005758,0.026215523,0.0002790719],"about_ca_topic_score_codex":0.8705352,"about_ca_topic_score_gemma":0.9938113,"teacher_disagreement_score":0.4804171,"about_ca_system_score_codex":0.0000050523045,"about_ca_system_score_gemma":0.0003096737,"threshold_uncertainty_score":0.9994364},"labels":[],"label_agreement":null},{"id":"W3104929171","doi":"10.1130/2017.0048(02)","title":"Late Cretaceous geology and fossils of Dinosaur Provincial Park","year":2017,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Paleontology and Evolutionary Biology","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":"Royal Tyrrell Museum","funders":"","keywords":"Cretaceous; Trophy; Taxon; Geography; Archaeology; Paleontology; Geology","score_opus":0.018965861950474238,"score_gpt":0.21412850281464224,"score_spread":0.195162640864168,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3104929171","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.039249487,0.0053238403,0.000098222816,0.00042763283,0.00025696846,0.00035288982,0.000297896,0.00004814823,0.9539449],"genre_scores_gemma":[0.7964156,0.0026139268,0.0042204997,0.001024912,0.00038223196,0.000004898743,0.00026186238,0.000010799986,0.19506526],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983917,0.000069542155,0.00045596113,0.0005020167,0.00016764556,0.00041313175],"domain_scores_gemma":[0.9983441,0.00034251402,0.0007893874,0.00032065695,0.00007628029,0.00012706636],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00020702978,0.0003253699,0.0009638,0.000031803465,0.00026378225,0.0000057538173,0.00040951086,0.0010693481,0.0013023521],"category_scores_gemma":[0.000053371223,0.00024697598,0.00035521056,0.000006622471,0.006489179,0.000031306263,0.000089608446,0.0005114561,0.000035830144],"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":[0.00068853865,0.00004509685,0.5001963,0.0002984787,0.0009455907,0.00009473654,0.0006430611,0.000049374576,0.00010995772,0.0053586275,0.0050279307,0.4865423],"study_design_scores_gemma":[0.00067709375,0.002422782,0.67710984,0.000067088076,0.00020408779,0.00013860811,0.000059970716,0.00075181073,0.000013432341,0.078216545,0.23962267,0.0007160927],"about_ca_topic_score_codex":0.0008282713,"about_ca_topic_score_gemma":0.00036074754,"teacher_disagreement_score":0.75887966,"about_ca_system_score_codex":0.000003838685,"about_ca_system_score_gemma":0.00010169887,"threshold_uncertainty_score":0.9999983},"labels":[],"label_agreement":null},{"id":"W3108144852","doi":"10.1130/2017.0048(01)","title":"Effects of sedimentary facies on structural styles in the Canadian Rocky Mountain Fold and Thrust Belt","year":2017,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological Modeling and 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":true,"ca_institutions":"ARC Resources (Canada)","funders":"","keywords":"Geology; Facies; Foreland basin; Fold (higher-order function); Hydrocarbon exploration; Sedimentary depositional environment; Sedimentary rock; Sedimentology; Thrust fault; Geomorphology; Terrane; Paleontology; Fault (geology); Stratigraphy; Fold and thrust belt; Tectonics; Petrology; Structural basin","score_opus":0.015604780919684622,"score_gpt":0.20612873147490948,"score_spread":0.19052395055522486,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3108144852","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.3438369,0.004529118,0.000048648726,0.0027960732,0.00015185594,0.0011452821,0.0006730269,0.000051216466,0.64676785],"genre_scores_gemma":[0.9913934,0.00026509864,0.0003444062,0.0019310322,0.000055390305,0.0000018568273,0.000119466415,0.0000035899004,0.00588579],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99853677,0.00006756318,0.00030536487,0.000376343,0.00036338935,0.00035059],"domain_scores_gemma":[0.99891526,0.00042517562,0.00023356336,0.00025912872,0.000036952144,0.00012991605],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021834736,0.00030101606,0.00063644786,0.000053848144,0.00036240293,0.000033123157,0.00047703212,0.00036245584,0.00042091685],"category_scores_gemma":[0.00003585193,0.00017014827,0.00031620645,0.000015733829,0.0011737361,0.000023672275,0.00004226414,0.00052134966,0.000008312804],"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":[0.00034511992,0.00008486568,0.20906906,0.0010290378,0.0019331366,0.00025918277,0.0070335646,0.009957352,0.00006447689,0.018133895,0.0061240364,0.74596626],"study_design_scores_gemma":[0.0020035964,0.0057677943,0.7627047,0.00077824335,0.0010369153,0.00003792225,0.0035310294,0.017718667,0.00011674182,0.13274893,0.07105084,0.0025046302],"about_ca_topic_score_codex":0.21768978,"about_ca_topic_score_gemma":0.043454356,"teacher_disagreement_score":0.74346167,"about_ca_system_score_codex":0.000011112536,"about_ca_system_score_gemma":0.00005383811,"threshold_uncertainty_score":0.9740001},"labels":[],"label_agreement":null},{"id":"W3114803663","doi":"10.1130/2017.0048(03)","title":"Lower to Middle Cambrian of the southern Canadian Rockies","year":2017,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological Studies and Exploration","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; Mount Royal University","funders":"","keywords":"Geology; Siliciclastic; Facies; Paleontology; Carbonate; Outcrop; Geochemistry; Geomorphology; Structural basin","score_opus":0.03401828756387045,"score_gpt":0.19124249605485552,"score_spread":0.15722420849098506,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3114803663","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.008390378,0.00036216542,0.000032726635,0.0020585523,0.0003000696,0.0004133731,0.00042182775,0.000021432132,0.9879995],"genre_scores_gemma":[0.597275,0.00013574032,0.0008503097,0.003265184,0.00020080087,0.0000034629827,0.00005269857,0.000008741894,0.39820805],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9986476,0.000023980296,0.00032025887,0.0003245415,0.00030553233,0.00037811397],"domain_scores_gemma":[0.9988132,0.00007988622,0.00038058407,0.00040453355,0.000109359644,0.0002124404],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00012798964,0.0002570363,0.00052621216,0.000017854989,0.0004732676,0.000020007348,0.000617651,0.0003258326,0.0025746676],"category_scores_gemma":[0.000053197407,0.00014710429,0.00050009496,0.000015165801,0.0010396873,0.000016979551,0.00010810936,0.00028547825,0.00023529661],"study_design_candidate":"not_applicable","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":[0.00042634722,0.000084874875,0.19243945,0.00038710856,0.0016888982,0.000044259737,0.014374575,0.002853767,0.000048229285,0.008849978,0.09009122,0.6887113],"study_design_scores_gemma":[0.000171994,0.00076369836,0.06303649,0.00012526834,0.00008279952,0.000003117616,0.0012396091,0.00013614759,0.0000081051985,0.016035309,0.9178895,0.00050798856],"about_ca_topic_score_codex":0.16270338,"about_ca_topic_score_gemma":0.099306844,"teacher_disagreement_score":0.82779825,"about_ca_system_score_codex":0.0000110089295,"about_ca_system_score_gemma":0.000086272485,"threshold_uncertainty_score":0.9983371},"labels":[],"label_agreement":null},{"id":"W3117110181","doi":"10.1130/2017.0045(02)","title":"Geology, stratigraphy, and paleontology of the Santa Ana Mountains, California, USA","year":2017,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geology and Paleoclimatology Research","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; Stratigraphy; Paleontology; Geologic time scale; Coastal plain; Geomorphology; Tectonics; Sedimentary rock","score_opus":0.025809094764608458,"score_gpt":0.2403285107753337,"score_spread":0.21451941601072524,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3117110181","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.09252191,0.004147221,0.000026324089,0.0006263227,0.0001624242,0.0005224951,0.00038676983,0.000024270543,0.90158224],"genre_scores_gemma":[0.9607756,0.0017341935,0.00090360874,0.00080729317,0.00006544804,0.0000034822772,0.000078704456,0.0000066189727,0.035625055],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99785864,0.0001789154,0.0005335743,0.0005611372,0.00030262847,0.0005650793],"domain_scores_gemma":[0.9976274,0.00064633886,0.00078943494,0.00067375496,0.00011689379,0.00014621837],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00038648766,0.00038238004,0.0010330594,0.000048804326,0.00047286574,0.000011436958,0.0009269346,0.0011691474,0.0028483467],"category_scores_gemma":[0.000066712026,0.00024353061,0.0005357712,0.000018991062,0.013064125,0.000026584019,0.00017801706,0.001057041,0.000053002757],"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":[0.00007829043,0.000009741716,0.9876987,0.00009076946,0.0002355223,0.000012154565,0.000090442,0.0000058727087,0.0000042225884,0.0024258841,0.0007247151,0.008623715],"study_design_scores_gemma":[0.0004481708,0.0009544549,0.90715337,0.00006236066,0.00015344677,0.00019253849,0.00018850066,0.00021526392,0.000012737586,0.04702143,0.0431741,0.00042365317],"about_ca_topic_score_codex":0.0016709919,"about_ca_topic_score_gemma":0.00604893,"teacher_disagreement_score":0.8682537,"about_ca_system_score_codex":0.0000015678227,"about_ca_system_score_gemma":0.00012992436,"threshold_uncertainty_score":0.9980632},"labels":[],"label_agreement":null},{"id":"W3167188828","doi":"10.1130/2021.2550(22)","title":"U-Pb geochronology of apatite crystallized within a terrestrial impact melt sheet: Manicouagan as a geochronometer test site","year":2021,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":"University of New Brunswick","funders":"","keywords":"Geochronology; Zircon; Apatite; Geology; Radiogenic nuclide; Overprinting; Geochemistry; Mineralogy; Crystallization; Metamorphic rock; Chemistry; Mantle (geology)","score_opus":0.014873567588454746,"score_gpt":0.21277927641125632,"score_spread":0.1979057088228016,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3167188828","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.43309012,0.003156863,0.00036798455,0.00074518693,0.00026293623,0.0009790057,0.001703492,0.00019377763,0.55950063],"genre_scores_gemma":[0.93492085,0.0005891863,0.009563901,0.0016035711,0.00039772078,0.000009750651,0.0017654303,0.000028061622,0.05112154],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9959317,0.00011577338,0.0013750877,0.0011065381,0.0006793483,0.00079158717],"domain_scores_gemma":[0.9964144,0.0010029634,0.0013485799,0.00065307954,0.00019340673,0.00038756392],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000304277,0.0008145793,0.0022881178,0.00009914209,0.0001464976,0.00003811465,0.00070012646,0.0010533124,0.07652531],"category_scores_gemma":[0.00024054678,0.0005619168,0.0024971191,0.00013431317,0.0025262095,0.000056185832,0.000270365,0.0009646086,0.0002456427],"study_design_candidate":"design_other","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":[0.007187617,0.002878094,0.2768929,0.0025409756,0.026724543,0.0016771471,0.006964131,0.015161777,0.05248138,0.0051534767,0.020182839,0.5821551],"study_design_scores_gemma":[0.017858211,0.048345976,0.15814938,0.002148832,0.009456379,0.0008674739,0.0025877345,0.048758462,0.0082644615,0.43452817,0.25383028,0.0152046345],"about_ca_topic_score_codex":0.0070157093,"about_ca_topic_score_gemma":0.00047514003,"teacher_disagreement_score":0.5669505,"about_ca_system_score_codex":0.000028850027,"about_ca_system_score_gemma":0.00022716307,"threshold_uncertainty_score":0.9996832},"labels":[],"label_agreement":null},{"id":"W3170237398","doi":"10.1130/2021.2550(06)","title":"Distinguishing friction- from shock-generated melt products in hypervelocity impact structures","year":2021,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","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":"University of New Brunswick","funders":"","keywords":"Anorthosite; Geology; Impact structure; Hypervelocity; Shock metamorphism; Shock (circulatory); Impact crater; Geochemistry; Gabbro; Petrology; Astrobiology; Igneous rock; Plagioclase","score_opus":0.023770117446125238,"score_gpt":0.209286175294299,"score_spread":0.18551605784817377,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3170237398","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5840996,0.004529244,0.00011751071,0.0008096398,0.00025483596,0.00043695213,0.0010849717,0.0001695672,0.4084977],"genre_scores_gemma":[0.9575006,0.00045879337,0.01543954,0.001124885,0.000448618,0.0000031707746,0.0030082362,0.000013443879,0.022002723],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9971698,0.00009486429,0.00070734555,0.0009771576,0.0005170253,0.00053379516],"domain_scores_gemma":[0.99832636,0.00040266913,0.00046235925,0.00036000067,0.00023572745,0.0002128724],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00017415915,0.0005397845,0.0012120634,0.000042378095,0.00017047762,0.000051884523,0.0004414322,0.0006303833,0.022088489],"category_scores_gemma":[0.00026498595,0.00036233157,0.0008836586,0.00015148576,0.0007248121,0.000039189,0.00013429225,0.0009825217,0.00003791675],"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":[0.00046069862,0.00025931798,0.5106043,0.00033518684,0.0035322886,0.00037933607,0.0015678904,0.01238882,0.0040547852,0.0020161753,0.008700638,0.45570055],"study_design_scores_gemma":[0.0010128982,0.0008914374,0.631735,0.00024710374,0.00063215307,0.000026115753,0.00063870044,0.012119002,0.0015319017,0.3068288,0.04156425,0.0027726435],"about_ca_topic_score_codex":0.02003223,"about_ca_topic_score_gemma":0.0005736477,"teacher_disagreement_score":0.45292792,"about_ca_system_score_codex":0.000025318146,"about_ca_system_score_gemma":0.00009911286,"threshold_uncertainty_score":0.9998829},"labels":[],"label_agreement":null},{"id":"W3183728144","doi":"10.1130/2021.0060(01)","title":"Cambrian–Lower Ordovician of SW Quebec–NE New York","year":2021,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Paleontology and Stratigraphy of Fossils","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":"University of Regina","funders":"","keywords":"Laurentia; Geology; Ordovician; Rift; Paleontology; Supercontinent; Rodinia; Onlap; Passive margin; Precambrian; Unconformity; Tectonics; Craton","score_opus":0.02471529726796141,"score_gpt":0.20971470805979328,"score_spread":0.18499941079183188,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3183728144","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0018494648,0.011041127,0.00020698551,0.00034780934,0.00026905633,0.0002053712,0.00014617074,0.000050705294,0.9858833],"genre_scores_gemma":[0.15700899,0.0010467484,0.023496369,0.0024738538,0.00075825164,0.0000026594123,0.00024922215,0.000012521955,0.81495136],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9978354,0.000060920764,0.0006719646,0.00056335406,0.00041337815,0.00045499875],"domain_scores_gemma":[0.9982698,0.00030991295,0.0006560946,0.00041304072,0.00009291084,0.00025826192],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001546409,0.00042584576,0.0011364758,0.000042003307,0.00014222061,0.00001579693,0.0004697273,0.0008834944,0.0055635003],"category_scores_gemma":[0.000024916624,0.00034589905,0.0011214993,0.000051200605,0.001987191,0.000031806452,0.000014465134,0.00066398445,0.000029906454],"study_design_candidate":"design_other","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":[0.00015695962,0.000043093303,0.022308059,0.00012331111,0.0008174208,0.00007082377,0.0006153068,0.000021074851,0.000066579545,0.009516717,0.013040516,0.9532201],"study_design_scores_gemma":[0.0007763285,0.0015916518,0.57826513,0.0003218291,0.00035670714,0.00003978734,0.0007033844,0.000111983914,0.00005032235,0.015616204,0.40096143,0.0012052332],"about_ca_topic_score_codex":0.013720597,"about_ca_topic_score_gemma":0.0101201525,"teacher_disagreement_score":0.9520149,"about_ca_system_score_codex":0.0000049537825,"about_ca_system_score_gemma":0.0003343197,"threshold_uncertainty_score":0.9998993},"labels":[],"label_agreement":null},{"id":"W3185613432","doi":"10.1130/fld060","title":"GSA in the Field in 2020","year":2021,"lang":"en","type":"book","venue":"Geological Society of America eBooks","topic":"Winter Sports Injuries and Performance","field":"Medicine","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":"","keywords":"TRIPS architecture; Geography; Salt lake; Section (typography); Archaeology; Coronavirus disease 2019 (COVID-19); History; Cartography; Geology; Engineering; Geomorphology; Advertising","score_opus":0.012266676257771843,"score_gpt":0.2652095156335907,"score_spread":0.25294283937581885,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3185613432","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.005921847,0.0011207075,0.000048626724,0.007204781,0.00012042769,0.00041326057,0.000008792384,0.000020230978,0.98514134],"genre_scores_gemma":[0.037623875,0.0020382488,0.0031844648,0.084953144,0.00079397584,0.000068952046,0.00014212381,0.000031371324,0.87116385],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9986759,0.00003203039,0.00044728498,0.00029346996,0.00027965129,0.0002716563],"domain_scores_gemma":[0.99911404,0.00026880333,0.00017584277,0.00035685953,0.000040816027,0.000043658158],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00021398586,0.00020653002,0.00069919537,0.000020225014,0.0000269596,0.0000071435634,0.00023789733,0.00040414036,0.0009934254],"category_scores_gemma":[0.000042870684,0.00012840073,0.00043847947,0.00007057553,0.00039305992,0.000010243991,0.0001392249,0.0011158347,0.000008059274],"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":[0.00019320445,0.00017541226,0.0092264665,0.000434187,0.000117533586,0.00036477827,0.004396175,0.0000041626126,0.000019426769,0.00041861858,0.9148174,0.06983267],"study_design_scores_gemma":[0.00045254393,0.00071977626,0.009215316,0.00040943787,0.00003910553,0.000033277505,0.0010418011,0.000055677392,0.000026073767,0.00073763623,0.98709315,0.00017619542],"about_ca_topic_score_codex":0.00013529311,"about_ca_topic_score_gemma":0.0000108705735,"teacher_disagreement_score":0.113977484,"about_ca_system_score_codex":0.0000536106,"about_ca_system_score_gemma":0.00019152531,"threshold_uncertainty_score":0.9999198},"labels":[],"label_agreement":null},{"id":"W3186147694","doi":"10.1130/2020.0060(02)","title":"From obduction to collision: A transect across Ordovician to Devonian sedimentary basins of the Québec Appalachians, Canada","year":2021,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Geology; Ordovician; Obduction; Transect; Devonian; Structural basin; Outcrop; Stratigraphy; Paleontology; Sedimentary rock; Sedimentary basin; Section (typography); Geomorphology; Tectonics; Oceanography; Subduction; Oceanic crust","score_opus":0.00988524286424747,"score_gpt":0.18670869017136746,"score_spread":0.17682344730712,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3186147694","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8539413,0.0009815831,0.00034291894,0.028858969,0.00053762103,0.0009993045,0.0064055757,0.00006167718,0.10787102],"genre_scores_gemma":[0.9156215,0.000067284534,0.005305363,0.0244423,0.00036593858,0.000008050199,0.00052709423,0.000013357958,0.053649098],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99755114,0.000071634066,0.000555319,0.0006796483,0.00068297284,0.00045929124],"domain_scores_gemma":[0.9985127,0.00028586548,0.00027712685,0.00042926281,0.00014160857,0.00035343456],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001195183,0.00038919787,0.00089488307,0.000016157066,0.0002546418,0.000015646492,0.00062893407,0.000303354,0.01055666],"category_scores_gemma":[0.000040490406,0.0002433759,0.0007738776,0.00015854619,0.0005502956,0.000015570557,0.00014461423,0.00048008378,0.00002472173],"study_design_candidate":"not_applicable","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":[0.0013005586,0.0004096686,0.28680137,0.00050705636,0.0054832497,0.00017078496,0.019347353,0.026076458,0.003690807,0.00039689476,0.12576176,0.53005403],"study_design_scores_gemma":[0.00040636538,0.00079997827,0.116090655,0.00023470963,0.00037271346,0.00000986603,0.005134293,0.0003612969,0.0012188556,0.0036160776,0.87068796,0.0010672136],"about_ca_topic_score_codex":0.9322986,"about_ca_topic_score_gemma":0.94667166,"teacher_disagreement_score":0.7449262,"about_ca_system_score_codex":0.000047081354,"about_ca_system_score_gemma":0.00046078858,"threshold_uncertainty_score":0.9924581},"labels":[],"label_agreement":null},{"id":"W3193873596","doi":"10.1130/2021.2551(01)","title":"Biostratigraphy, Age, and Paleoenvironment of the Pliocene Beaufort Formation on Meighen Island, Canadian Arctic Archipelago","year":2021,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Canadian Museum of Nature; Agriculture and Agri-Food Canada; Geological Survey of Canada; University of Lethbridge","funders":"","keywords":"Geology; Arctic; Neogene; Paleontology; Archipelago; Bay; Oceanography; Structural basin","score_opus":0.01917344248287968,"score_gpt":0.20004234076817387,"score_spread":0.18086889828529418,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3193873596","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.18973026,0.0020288297,0.000026611722,0.0018853252,0.00017673142,0.00086515845,0.0005970829,0.000017610155,0.8046724],"genre_scores_gemma":[0.9864418,0.00081628066,0.00044117053,0.0012344967,0.000023487639,0.0000026367607,0.00027159174,0.000003910789,0.010764649],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985766,0.000091657705,0.00034185394,0.00031952522,0.00029884826,0.00037153348],"domain_scores_gemma":[0.99890697,0.00033869,0.00024404617,0.00029584978,0.000045503326,0.00016894276],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00017837963,0.00023946076,0.0004711107,0.000054613447,0.00022418004,0.000008994828,0.00028000874,0.00043439723,0.0016461009],"category_scores_gemma":[0.000028717152,0.00015593876,0.00031913986,0.000033067743,0.0022882493,0.000017453898,0.0000471212,0.00061484776,0.000017583925],"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":[0.000055732195,0.000019915415,0.97315323,0.00020887116,0.00029124855,0.000049895152,0.0008434663,0.00008514461,0.000007524498,0.0027735091,0.0007261558,0.021785276],"study_design_scores_gemma":[0.0003797183,0.0008403743,0.9616455,0.00016537185,0.000116191986,0.00006805637,0.0004376613,0.00020472091,0.00006140143,0.01919047,0.0165187,0.00037186785],"about_ca_topic_score_codex":0.0067539345,"about_ca_topic_score_gemma":0.040462345,"teacher_disagreement_score":0.7967115,"about_ca_system_score_codex":0.0000040949503,"about_ca_system_score_gemma":0.00007755813,"threshold_uncertainty_score":0.99986017},"labels":[],"label_agreement":null},{"id":"W3194093291","doi":"10.1130/2021.2552(06)","title":"Numerical models of Cretaceous continental collision and slab breakoff dynamics in western Canada","year":2021,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Eclogitization; Geology; Subduction; Lithosphere; Craton; Collision zone; Continental collision; Mantle (geology); Magmatism; Foreland basin; Continental crust; Slab window; Convergent boundary; Fibrous joint; Slab; Geophysics; Oceanic crust; Seismology; Tectonics","score_opus":0.00976279031668476,"score_gpt":0.17503566681876864,"score_spread":0.1652728765020839,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3194093291","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.38900217,0.005354267,0.0006296493,0.0015616253,0.0001341944,0.00055011344,0.0011374261,0.000050599378,0.60157996],"genre_scores_gemma":[0.9563493,0.0006982124,0.0022227555,0.0010274097,0.0000375282,0.0000016864955,0.00054333487,0.000007813416,0.039111927],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9977995,0.00005358259,0.000691503,0.000572541,0.0005019206,0.0003809103],"domain_scores_gemma":[0.9986835,0.00037193362,0.00041078273,0.00021297272,0.00011913545,0.00020164486],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00011656166,0.0003669851,0.0012402129,0.000028441096,0.00005859437,0.000012189341,0.00027523402,0.00041142965,0.002044223],"category_scores_gemma":[0.00002569414,0.0002727867,0.00038994203,0.00006913877,0.00085558515,0.000026892973,0.00012223027,0.0005095546,0.000004192543],"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":[0.0007212823,0.00029228537,0.80296534,0.00089003023,0.0014746867,0.0006187506,0.0005261861,0.01977602,0.00016577121,0.005895649,0.0029219587,0.16375203],"study_design_scores_gemma":[0.003768337,0.0033047579,0.12420465,0.0010295816,0.001054205,0.00032920882,0.0032297058,0.64470464,0.0005785059,0.15219995,0.060736377,0.0048600673],"about_ca_topic_score_codex":0.34440416,"about_ca_topic_score_gemma":0.14539042,"teacher_disagreement_score":0.6787607,"about_ca_system_score_codex":0.000032030093,"about_ca_system_score_gemma":0.00014544441,"threshold_uncertainty_score":0.9999724},"labels":[],"label_agreement":null},{"id":"W3210333309","doi":"10.1130/2021.2554(15)","title":"Testing petrogenetic models for contemporaneous mafic and felsic to intermediate magmatism within the “Newer Granite” suite of the Scottish and Irish Caledonides","year":2022,"lang":"en","type":"article","venue":"Geological Society of America eBooks","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":"St. Francis Xavier University","funders":"","keywords":"Mafic; Felsic; Geochemistry; Magmatism; Irish; Suite; Geology; Petrology; Archaeology; Paleontology; Geography","score_opus":0.021188813425522927,"score_gpt":0.19844435110403166,"score_spread":0.17725553767850874,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3210333309","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967031,0.000657406,0.00031135508,0.0009824771,0.000037818925,0.0003794041,0.00013834359,0.000016236569,0.00077389035],"genre_scores_gemma":[0.99393183,0.000011272472,0.0038626525,0.0019691014,0.000018631203,0.000016939151,0.000010870878,0.0000025654747,0.0001761573],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987104,0.00013858096,0.00033788846,0.00029933354,0.00025337932,0.0002604517],"domain_scores_gemma":[0.9985661,0.0008833515,0.00022635837,0.00015543666,0.000068753136,0.00009999601],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003659726,0.00014584127,0.00034408722,0.000014022052,0.00038364742,0.000020294,0.0003312782,0.000046343957,0.00019137881],"category_scores_gemma":[0.00016705802,0.00007618256,0.00018809538,0.00017511279,0.0011001942,0.000018345943,0.0002247643,0.0002098586,6.630808e-7],"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":[0.00027156732,0.00010322999,0.793758,0.00019314047,0.00030743497,0.000008065657,0.0044822847,0.030090492,0.0039322,0.00020323026,0.0020582406,0.16459216],"study_design_scores_gemma":[0.0008716217,0.0021420429,0.7065936,0.00005006509,0.0002502407,0.000090971436,0.0051319706,0.1816057,0.0004800393,0.10114957,0.0011124554,0.0005217703],"about_ca_topic_score_codex":0.002416865,"about_ca_topic_score_gemma":0.00011812153,"teacher_disagreement_score":0.1640704,"about_ca_system_score_codex":0.0000030003773,"about_ca_system_score_gemma":0.000017957911,"threshold_uncertainty_score":0.40537116},"labels":[],"label_agreement":null},{"id":"W4200028261","doi":"10.1130/2021.2553(30)","title":"Dense melt residues drive mid-ocean-ridge “hotspots”","year":2021,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":"McMaster University","funders":"","keywords":"Mantle (geology); Geology; Hotspot (geology); Upwelling; Mid-ocean ridge; Plume; Buoyancy; Geophysics; Mantle convection; Mantle wedge; Mantle plume; Partial melting; Thermal; Petrology; Crust; Subduction; Lithosphere; Tectonics; Mechanics; Seismology; Thermodynamics; Oceanography; Physics","score_opus":0.017727884971023865,"score_gpt":0.20788701864502046,"score_spread":0.1901591336739966,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200028261","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.032628443,0.002359029,0.000081030696,0.00051297655,0.00079354114,0.00056627736,0.0016341553,0.00019889978,0.9612256],"genre_scores_gemma":[0.17760658,0.0032736058,0.011740982,0.0048902887,0.0016253323,0.0000056149042,0.0018663668,0.00006452812,0.7989267],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99738085,0.000086202344,0.0006181358,0.0007679457,0.00058291195,0.0005639563],"domain_scores_gemma":[0.9981502,0.0003436721,0.00056222186,0.00051777327,0.00019063069,0.00023544735],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00022485336,0.0005382074,0.0012013604,0.00003220035,0.00022016573,0.000064730986,0.0005150932,0.00063789514,0.009752072],"category_scores_gemma":[0.000029930208,0.00042357488,0.00080153963,0.000036386482,0.0011414847,0.000044172753,0.00015167127,0.00046992002,0.00029205007],"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":[0.00090474205,0.0003448984,0.009634603,0.002228333,0.0069980696,0.0012717362,0.0074217278,0.001337811,0.009378936,0.054073505,0.54211676,0.36428887],"study_design_scores_gemma":[0.0004916728,0.00074861135,0.010046745,0.00022685667,0.00035393273,0.000024172688,0.00031948363,0.000081153514,0.0016015059,0.029089788,0.95572126,0.0012948129],"about_ca_topic_score_codex":0.0010984854,"about_ca_topic_score_gemma":0.000042668562,"teacher_disagreement_score":0.4136045,"about_ca_system_score_codex":0.000007692134,"about_ca_system_score_gemma":0.00012744979,"threshold_uncertainty_score":0.9998216},"labels":[],"label_agreement":null},{"id":"W4200045066","doi":"10.1130/2021.2554(04)","title":"New detrital zircon U-Pb ages and Lu-Hf isotopic data from metasedimentary rocks along the western boundary of the composite Avalon terrane in the southeastern New England Appalachians","year":2021,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","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":"","keywords":"Terrane; Zircon; Geology; Laurentia; Provenance; Gondwana; Geochemistry; Ordovician; Devonian; Paleontology; Tectonics","score_opus":0.025614608647938776,"score_gpt":0.20620217365057852,"score_spread":0.18058756500263975,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200045066","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.83033407,0.04767815,0.0041608857,0.028292235,0.000589289,0.002512767,0.0050616404,0.00011191563,0.081259035],"genre_scores_gemma":[0.9482139,0.0009458132,0.0045636045,0.009221213,0.00068968977,0.000003465562,0.0030391007,0.000016232792,0.033307035],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9975306,0.00023210375,0.00061821094,0.0006784784,0.00058352994,0.00035710202],"domain_scores_gemma":[0.9975987,0.00097456964,0.00042060547,0.00083389477,0.000029668196,0.00014253068],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00031486963,0.0004113524,0.00085144566,0.000021538279,0.00021461524,0.00006956085,0.0015021954,0.00029944006,0.0021105057],"category_scores_gemma":[0.000027765715,0.00018542631,0.00049041765,0.00007524797,0.0012166421,0.0000590891,0.0005297289,0.00087254605,0.000013138835],"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":[0.00022300881,0.00009916099,0.7950009,0.00012529019,0.0015350945,0.00006261298,0.0048202085,0.00018130042,0.0008564345,0.000043577988,0.0037284272,0.19332395],"study_design_scores_gemma":[0.004278792,0.0013043887,0.7049214,0.00066592084,0.0032976386,0.00014221205,0.004438031,0.0017389139,0.0006147371,0.057481032,0.21917792,0.0019390088],"about_ca_topic_score_codex":0.05114614,"about_ca_topic_score_gemma":0.010175132,"teacher_disagreement_score":0.2154495,"about_ca_system_score_codex":0.0000036098045,"about_ca_system_score_gemma":0.00007216345,"threshold_uncertainty_score":0.9988017},"labels":[],"label_agreement":null},{"id":"W4200267630","doi":"10.1130/2021.0062(07)","title":"Upper Grand Coulee: New views of a channeled scabland megafloods enigma","year":2021,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geology and Paleoclimatology Research","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":"Government of Saskatchewan","funders":"","keywords":"Geology; Geomorphology; Drumlin; Hydrology (agriculture); Oceanography; Ice stream","score_opus":0.03858713389925278,"score_gpt":0.2503088630470394,"score_spread":0.21172172914778664,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200267630","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.01154585,0.011820415,0.00031026563,0.0011289014,0.00026158887,0.0006110403,0.00017340269,0.000059146852,0.9740894],"genre_scores_gemma":[0.17265797,0.00588953,0.00910853,0.0025039073,0.0003883205,0.000007340925,0.0008443533,0.000027543792,0.80857253],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99735326,0.00016084657,0.0007094302,0.00065325137,0.0004922695,0.0006309294],"domain_scores_gemma":[0.99794585,0.0006328356,0.00051621435,0.00044260858,0.00017446844,0.00028804273],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00042227688,0.00044843613,0.0015365464,0.00006530817,0.00017632007,0.000013144413,0.00053311925,0.0011179022,0.01791576],"category_scores_gemma":[0.000057125264,0.0003390037,0.0009123763,0.0000629722,0.0025099728,0.000029907638,0.000113129856,0.000947019,0.0001558225],"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":[0.00070848886,0.00010524394,0.87225705,0.0007636055,0.0020765166,0.00017960314,0.0018413666,0.000108452885,0.00006634498,0.004697353,0.03540655,0.08178943],"study_design_scores_gemma":[0.0036854628,0.00311469,0.05275905,0.0005621122,0.000717651,0.00042385573,0.00067612616,0.0014477102,0.00036455275,0.05152808,0.8826659,0.0020548557],"about_ca_topic_score_codex":0.00026492836,"about_ca_topic_score_gemma":0.00020383843,"teacher_disagreement_score":0.8472593,"about_ca_system_score_codex":0.0000022911477,"about_ca_system_score_gemma":0.0002543692,"threshold_uncertainty_score":0.9999062},"labels":[],"label_agreement":null},{"id":"W4200410695","doi":"10.1130/spe554","title":"New Developments in the Appalachian-Caledonian-Variscan Orogen","year":2021,"lang":"en","type":"book","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","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":"","keywords":"Terrane; Geology; Paleontology; Field (mathematics); Archaeology; Earth science; Oceanography; Geography; Tectonics","score_opus":0.014367455102311775,"score_gpt":0.19370171039589354,"score_spread":0.17933425529358177,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200410695","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.005110476,0.0020273407,0.0002722553,0.0014954478,0.000082800936,0.0003392857,0.00006748113,0.00004883525,0.99055606],"genre_scores_gemma":[0.10847825,0.0010719411,0.049446303,0.02157543,0.00072290975,0.000018609964,0.0022643874,0.000021448957,0.8164007],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9970435,0.00019256247,0.0006881659,0.00071353914,0.00071093824,0.0006512915],"domain_scores_gemma":[0.99841785,0.0005428175,0.00034930976,0.00039006068,0.00007150456,0.00022842875],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00034574518,0.00045305403,0.0009789602,0.000037304402,0.00014506592,0.0000437116,0.0010141673,0.0005695474,0.013882414],"category_scores_gemma":[0.00006313064,0.00026028903,0.000840078,0.00024978828,0.0006968546,0.000024807829,0.0001392999,0.0009881546,0.0002079149],"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":[0.00008718025,0.00015869073,0.24476576,0.00017971809,0.00086031435,0.00017374268,0.00211806,0.00043492793,0.00002805119,0.0006521787,0.17066118,0.5798802],"study_design_scores_gemma":[0.000544538,0.0003510489,0.16821511,0.00010508337,0.0002266009,0.000034415945,0.0009944551,0.00031100903,0.00003390391,0.07565372,0.752579,0.000951121],"about_ca_topic_score_codex":0.003343891,"about_ca_topic_score_gemma":0.00063937897,"teacher_disagreement_score":0.5819178,"about_ca_system_score_codex":0.000017028333,"about_ca_system_score_gemma":0.0003963603,"threshold_uncertainty_score":0.9999849},"labels":[],"label_agreement":null},{"id":"W4200611218","doi":"10.1130/2021.2553(07)","title":"The African continental divide: Indian versus Atlantic Ocean spreading during Gondwana dispersal","year":2021,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological formations and processes","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":"McMaster University","funders":"","keywords":"Seafloor spreading; Gondwana; Geology; Biological dispersal; Plate tectonics; Indian ocean; Continental drift; Oceanography; Ridge; Paleontology; Tectonics; Deep sea; Breakup; Population","score_opus":0.016279378467377977,"score_gpt":0.20152341857095477,"score_spread":0.18524404010357678,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200611218","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.15853244,0.0027717995,0.00008675249,0.0012398573,0.000574882,0.0005017354,0.00025915063,0.00016955685,0.8358638],"genre_scores_gemma":[0.95719606,0.0008950463,0.00038489557,0.00023108975,0.00018928347,0.0000014819408,0.0002954665,0.000009023796,0.04079763],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99799305,0.000048204725,0.0005121968,0.00043919418,0.00043950145,0.0005678703],"domain_scores_gemma":[0.99823606,0.0007618093,0.00042411487,0.00028818892,0.00009411023,0.00019574536],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00018361444,0.0003820312,0.0005784009,0.000027077935,0.00077149586,0.00010478945,0.0005321484,0.00033398514,0.0031368218],"category_scores_gemma":[0.00008369194,0.0002362899,0.00057574944,0.000061709565,0.0015214825,0.00006078154,0.00014382396,0.0006196201,0.00008825619],"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":[0.002416107,0.00021018318,0.23246545,0.0017061994,0.00501847,0.0005577812,0.012635877,0.0012260923,0.00010494832,0.037165053,0.02088822,0.68560565],"study_design_scores_gemma":[0.0028271268,0.0025682289,0.08595007,0.00053200114,0.000645395,0.00018212854,0.01693751,0.0014771589,0.00013868877,0.014493096,0.871191,0.003057569],"about_ca_topic_score_codex":0.0011471229,"about_ca_topic_score_gemma":0.0002254296,"teacher_disagreement_score":0.8503028,"about_ca_system_score_codex":0.000013872025,"about_ca_system_score_gemma":0.00006426274,"threshold_uncertainty_score":0.9977744},"labels":[],"label_agreement":null},{"id":"W4206339973","doi":"10.1130/2021.2554(10)","title":"A reevaluation of the tectonic history of the Dashwoods terrane using in situ and isotope-dilution U-Pb geochronology, western Newfoundland","year":2022,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":"","keywords":"Terrane; Ordovician; Geology; Detritus; Orogeny; Geochronology; Paleontology; Back-arc basin; Geochemistry; Laurentia; Tectonics; Subduction","score_opus":0.03130728463778544,"score_gpt":0.21271547164745058,"score_spread":0.18140818700966516,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4206339973","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.84034294,0.0040887157,0.00006388747,0.0010897465,0.00021674874,0.00067994936,0.000085283595,0.00002110726,0.15341163],"genre_scores_gemma":[0.98731375,0.00021197219,0.0005213316,0.00050106033,0.000029364839,0.0000026972525,0.000033980374,0.0000040462414,0.011381829],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982609,0.0001712108,0.00055347715,0.000371221,0.0004094155,0.00023374488],"domain_scores_gemma":[0.9986181,0.00021874915,0.0007374259,0.0003244079,0.000058154954,0.000043139513],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00034505944,0.00023002466,0.00064244174,0.000034980494,0.00009611651,0.000003243731,0.00043401364,0.00029049144,0.0036704405],"category_scores_gemma":[0.000048430382,0.00012678717,0.00048236098,0.000071675495,0.002410013,0.000025632504,0.00026722328,0.00055538677,0.0000017525579],"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":[0.00038076463,0.00018716248,0.8629183,0.000521008,0.00074706465,0.0000059350596,0.0030116187,0.0067814435,0.019926421,0.0012721159,0.00046709308,0.10378106],"study_design_scores_gemma":[0.0011870293,0.0011564757,0.8763739,0.00024315057,0.00073635747,0.000042977485,0.00038253397,0.009342371,0.00023965583,0.043688986,0.06585622,0.00075034186],"about_ca_topic_score_codex":0.009007569,"about_ca_topic_score_gemma":0.0026122986,"teacher_disagreement_score":0.14697078,"about_ca_system_score_codex":0.00006929887,"about_ca_system_score_gemma":0.00012691543,"threshold_uncertainty_score":0.99759156},"labels":[],"label_agreement":null},{"id":"W4210851680","doi":"10.1130/2021.2553(14)","title":"Detrital zircon record of the Mesoproterozoic Belt basin and implications for horizontal and vertical tectonic models","year":2022,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":"","keywords":"Geology; Supercontinent; Rift; Zircon; Proterozoic; Paleontology; Tectonics; Craton; Structural basin","score_opus":0.021123729337295706,"score_gpt":0.1975551757659492,"score_spread":0.1764314464286535,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4210851680","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.49460763,0.0073948633,0.00561315,0.012691075,0.0002493752,0.004037626,0.0030602992,0.00017773738,0.47216827],"genre_scores_gemma":[0.98384273,0.0005928943,0.009471613,0.0009252245,0.00005948576,0.00002790467,0.00015378527,0.000008825424,0.0049175215],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99854386,0.00003786594,0.00042541247,0.00048583339,0.00021770378,0.00028931248],"domain_scores_gemma":[0.9988546,0.0004957006,0.00021463507,0.00023765027,0.000068170324,0.0001292686],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00014959722,0.00025663275,0.00063763116,0.000022926968,0.0002548168,0.000011382808,0.00030479874,0.00026515705,0.0014290446],"category_scores_gemma":[0.000045773955,0.00015826225,0.0005640687,0.000049763552,0.001558782,0.000030312362,0.00020525667,0.00040440346,0.0000012050898],"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":[0.000714092,0.0002258187,0.09047449,0.00062457926,0.0015763049,0.0000041579588,0.0005942205,0.00034103935,0.0062227207,0.06624999,0.0025166816,0.8304559],"study_design_scores_gemma":[0.0008284685,0.0027970765,0.05420389,0.000054753567,0.000673391,0.00003886237,0.0001924755,0.0047765626,0.00046002216,0.90004903,0.035116732,0.0008087302],"about_ca_topic_score_codex":0.0010276029,"about_ca_topic_score_gemma":0.00008617431,"teacher_disagreement_score":0.83379906,"about_ca_system_score_codex":0.000007509195,"about_ca_system_score_gemma":0.000032654836,"threshold_uncertainty_score":0.99948376},"labels":[],"label_agreement":null},{"id":"W4210974420","doi":"10.1130/dnag-gna-p1.41","title":"Stratiform Iron","year":2015,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Minerals Flotation and Separation Techniques","field":"Environmental Science","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":"Mineral; Section (typography); Volume (thermodynamics); Mineral deposit; Geology; Mineralogy; Mining engineering; Computer science; Geochemistry; Metallurgy; Materials science","score_opus":0.037158934429271845,"score_gpt":0.26102798458705717,"score_spread":0.22386905015778533,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4210974420","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00019804692,0.00004827304,0.0010990596,0.00017721354,0.000025948406,0.00024335476,0.00001691086,0.00012414901,0.998067],"genre_scores_gemma":[0.0065888925,0.00009936687,0.017789325,0.0017376143,0.000056434357,0.00001850849,0.000059535392,0.000022309416,0.97362804],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9986419,0.000015127384,0.00037269943,0.00032788722,0.00045312312,0.00018924072],"domain_scores_gemma":[0.99923515,0.000033939115,0.00032761868,0.00024673456,0.000028500312,0.00012804063],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000142619,0.00024518254,0.00037406466,0.000010495847,0.00006162498,0.0000100004245,0.00023961124,0.00035299576,0.015557514],"category_scores_gemma":[0.000008886778,0.00019609112,0.00028850633,0.000014641662,0.0009886061,0.00003342683,0.00018548623,0.00027074298,0.00046478337],"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":[0.000028130227,0.000048170827,0.000067867404,0.000028206663,0.000047300426,0.0000046381106,0.0008057818,0.00007298444,0.0024198357,0.02917785,0.7908834,0.1764158],"study_design_scores_gemma":[0.0001215053,0.00034521188,0.00005688078,0.000011264768,0.000020016612,0.000003503343,0.00006831816,0.00024900291,0.000251989,0.03546135,0.9631264,0.0002845588],"about_ca_topic_score_codex":0.00008480775,"about_ca_topic_score_gemma":0.000003981243,"teacher_disagreement_score":0.17613125,"about_ca_system_score_codex":0.000096194155,"about_ca_system_score_gemma":0.000019014895,"threshold_uncertainty_score":0.9853424},"labels":[],"label_agreement":null},{"id":"W4211054542","doi":"10.1130/dnag-gna-f1.681","title":"Metallogeny","year":2015,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","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":"","keywords":"Paleozoic; Geology; Metallogeny; Mesozoic; Graben; Paleontology; Devonian; Earth science; Structural basin","score_opus":0.04319358598697458,"score_gpt":0.23407706470563983,"score_spread":0.19088347871866523,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4211054542","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000004999938,0.0006224354,0.030767445,0.0013840044,0.0001182514,0.00017396203,0.000008909685,0.00022536321,0.96669465],"genre_scores_gemma":[0.0036855305,0.00008726216,0.06430822,0.0017510166,0.00014255442,0.000013571614,0.000020824216,0.000009345402,0.92998165],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.9977362,0.000030331621,0.0005007774,0.0007570482,0.0005320536,0.000443593],"domain_scores_gemma":[0.99782157,0.00013818983,0.0005543933,0.0008991181,0.0003715241,0.0002151785],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.00033867682,0.0004423615,0.00084155175,0.000024541192,0.00009929004,0.000027420545,0.0015478814,0.00068793487,0.00055844005],"category_scores_gemma":[0.000061411156,0.00035834426,0.0007924805,0.00003612574,0.0009589216,0.000041390816,0.001252195,0.00061259104,0.00011500967],"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":[0.000019093206,0.000074920164,0.000019605624,0.00019866189,0.00072838116,0.0000661355,0.00085886306,0.00012744618,0.00089261157,0.6335432,0.20543382,0.15803728],"study_design_scores_gemma":[0.00013106284,0.00017191378,0.000005614422,0.000025759884,0.00003054647,0.000021479325,0.000028520279,0.000605759,0.00012048568,0.2062219,0.79229236,0.000344611],"about_ca_topic_score_codex":0.000013766272,"about_ca_topic_score_gemma":1.3311548e-7,"teacher_disagreement_score":0.5868586,"about_ca_system_score_codex":0.00004569962,"about_ca_system_score_gemma":0.00013221466,"threshold_uncertainty_score":0.9998869},"labels":[],"label_agreement":null},{"id":"W4214814335","doi":"10.1130/2022.2557(18)","title":"Impact-crater ages and micrometeorite paleofluxes compared: Evidence for the importance of ordinary chondrites in the flux of meteorites and asteroids to Earth over the past 500 million years","year":2022,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Astro and Planetary Science","field":"Physics and Astronomy","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":"Impact crater; Meteorite; Asteroid; Parent body; Geology; Breakup; Astrobiology; Chondrite; Flux (metallurgy); Paleontology; Physics; Chemistry","score_opus":0.029033119897350988,"score_gpt":0.26524896161155803,"score_spread":0.23621584171420704,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4214814335","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99197525,0.0030273418,0.0002862099,0.00039216303,0.000051216277,0.00093658175,0.0006400621,0.0000055867113,0.002685568],"genre_scores_gemma":[0.9931922,0.00018489092,0.0023230605,0.00036429247,0.00008473032,0.000035440073,0.000055744993,0.000010403171,0.0037492586],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998742,0.00007549018,0.00036986812,0.00032003806,0.00025665984,0.00023595057],"domain_scores_gemma":[0.9976125,0.001632293,0.00036586143,0.00030195198,0.00004377777,0.000043660653],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044643303,0.0002370041,0.0004897877,0.00002814955,0.00013907626,0.00002363335,0.00044682974,0.000060049973,0.0003579634],"category_scores_gemma":[0.00000966553,0.00011884065,0.0002696206,0.00006286681,0.0010961352,0.00004989425,0.00023457577,0.0003062946,5.8750294e-7],"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":[0.00031378458,0.000075166965,0.9100367,0.0001537311,0.00053698046,0.0000029340265,0.0069565778,0.00021107824,0.007493086,0.0018307611,0.006395733,0.06599346],"study_design_scores_gemma":[0.00036574175,0.0016094403,0.9580883,0.0001418222,0.00015311637,0.000004756728,0.0022758795,0.00022967557,0.00007661115,0.0017075007,0.035032544,0.00031464675],"about_ca_topic_score_codex":0.00030810537,"about_ca_topic_score_gemma":0.000007270124,"teacher_disagreement_score":0.06567881,"about_ca_system_score_codex":0.00000526274,"about_ca_system_score_gemma":0.000024310953,"threshold_uncertainty_score":0.48461813},"labels":[],"label_agreement":null},{"id":"W4220674500","doi":"10.1130/2021.2555(10)","title":"Linking the Gulf of Mexico and Coast Mountains batholith during late Paleocene time: Insights from Hf isotopes in detrital zircons","year":2022,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":"","keywords":"Batholith; Geology; Geochronology; Cenozoic; Structural basin; Mesozoic; Paleontology; Provenance; Geochemistry; Tectonics","score_opus":0.010232005179281217,"score_gpt":0.17712701354265453,"score_spread":0.16689500836337332,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220674500","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.88560724,0.0028806466,0.000019790434,0.00041704846,0.000034550252,0.00027798006,0.0004481548,0.00003862737,0.11027596],"genre_scores_gemma":[0.9904839,0.00077397097,0.001090612,0.00063328724,0.000063949155,0.000004176294,0.00025975742,0.000006798157,0.006683565],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99788886,0.00009669475,0.0006260071,0.0005740347,0.000449551,0.00036484204],"domain_scores_gemma":[0.99838036,0.00072201906,0.0004505763,0.00026770425,0.00005550541,0.00012383463],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00015913446,0.00036565255,0.00093235954,0.00005306873,0.00023759819,0.000019822424,0.00045566508,0.00032377447,0.0071479026],"category_scores_gemma":[0.000038190505,0.0002233427,0.0004923803,0.00009649205,0.0015670683,0.000040256866,0.00030647658,0.00081895036,0.000017562257],"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":[0.00060498517,0.0002661592,0.87277853,0.00031740396,0.0017796643,0.00024141929,0.006661847,0.006366692,0.0066253203,0.0026297653,0.00029906727,0.10142914],"study_design_scores_gemma":[0.002290535,0.0016526926,0.6389238,0.00043869214,0.000784371,0.00003704609,0.002235648,0.0073114727,0.0018398211,0.29410914,0.04797447,0.00240228],"about_ca_topic_score_codex":0.0040238705,"about_ca_topic_score_gemma":0.00048428218,"teacher_disagreement_score":0.29147935,"about_ca_system_score_codex":0.000009448185,"about_ca_system_score_gemma":0.000029303714,"threshold_uncertainty_score":0.9937597},"labels":[],"label_agreement":null},{"id":"W4220937441","doi":"10.1130/2021.2554(05)","title":"U-Pb detrital zircon analysis of sedimentary rocks of the southeastern New England Avalon terrane in the U.S. Appalachians: Evidence for a separate crustal block","year":2022,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","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":"","keywords":"Zircon; Terrane; Geology; Geochemistry; Archean; Provenance; Geochronology; Craton; Proterozoic; Metamorphic rock; Tectonics; Paleontology","score_opus":0.0363967216962774,"score_gpt":0.2320872501550733,"score_spread":0.19569052845879592,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220937441","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.82029796,0.010477388,0.0026498507,0.0068653,0.00035802543,0.0042782207,0.0037801054,0.00009093175,0.15120222],"genre_scores_gemma":[0.9872213,0.00021018571,0.001389417,0.0012928225,0.00009208923,0.000010653559,0.00026027812,0.000006149026,0.009517102],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99731225,0.00016451905,0.00086276646,0.0005500089,0.00072600413,0.00038443063],"domain_scores_gemma":[0.99715877,0.0014076908,0.00082195725,0.0004365432,0.000074548836,0.000100500394],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005395198,0.0003664045,0.0011928421,0.00009020284,0.00014168602,0.000011888303,0.0009844279,0.00027036562,0.004893248],"category_scores_gemma":[0.00007921566,0.00019352218,0.001987251,0.0003002058,0.00096553325,0.000034238892,0.00017115724,0.00059100555,0.0000037381678],"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":[0.0036161367,0.0006396857,0.76960284,0.0010269044,0.014924104,0.00003659606,0.018724179,0.06523983,0.0039357245,0.0005885705,0.0033248023,0.11834063],"study_design_scores_gemma":[0.01286457,0.019468367,0.43401435,0.0014981093,0.045615945,0.000110305875,0.019933864,0.07282894,0.0042152256,0.14555797,0.23713595,0.0067563886],"about_ca_topic_score_codex":0.011023124,"about_ca_topic_score_gemma":0.0012967754,"teacher_disagreement_score":0.33558849,"about_ca_system_score_codex":0.000007979038,"about_ca_system_score_gemma":0.0000725012,"threshold_uncertainty_score":0.99601644},"labels":[],"label_agreement":null},{"id":"W4220979701","doi":"10.1130/2021.2554(01)","title":"Paleozoic orogenies and relative plate motions at the sutures of the Iapetus-Rheic Ocean","year":2022,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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 Calgary","funders":"","keywords":"Gondwana; Geology; Laurentia; Paleontology; Paleozoic; Plate tectonics; Supercontinent; Ordovician; Subduction; Craton; Passive margin; Seafloor spreading; Baltica; Rift; Convergent boundary; Oceanic crust; Tectonics","score_opus":0.013502295053183297,"score_gpt":0.1800124162054181,"score_spread":0.16651012115223482,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220979701","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.22978872,0.008363897,0.000022169728,0.005334538,0.00014789564,0.0006697694,0.00096958445,0.000072259114,0.75463116],"genre_scores_gemma":[0.8504236,0.0016969034,0.0005051252,0.0019522617,0.000074601565,0.0000037020486,0.00018531957,0.000007919351,0.14515059],"study_design_codex":"observational","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99822605,0.000113706505,0.00044580805,0.00043901626,0.00047167626,0.00030371879],"domain_scores_gemma":[0.9981751,0.00078961934,0.0005331033,0.00034191125,0.00006439246,0.0000958859],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00019804781,0.00031557158,0.0006121852,0.000017429993,0.00060385786,0.000010123834,0.00051469257,0.00025505997,0.024273513],"category_scores_gemma":[0.00006913996,0.00014484064,0.0009594661,0.00007447824,0.003884733,0.00002303612,0.00040237262,0.00071984,0.000019748026],"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":[0.00072328077,0.0003207915,0.6320489,0.00060719106,0.010713614,0.000056497276,0.011228149,0.010353598,0.00075611327,0.10401517,0.041822065,0.18735461],"study_design_scores_gemma":[0.00051502686,0.0011510954,0.19738722,0.000073951975,0.0012435248,0.00005771257,0.0014544736,0.0011156987,0.00019535937,0.40456533,0.39121833,0.0010222753],"about_ca_topic_score_codex":0.0007931157,"about_ca_topic_score_gemma":0.00019008006,"teacher_disagreement_score":0.62063485,"about_ca_system_score_codex":0.0000078618095,"about_ca_system_score_gemma":0.000026225502,"threshold_uncertainty_score":0.99882615},"labels":[],"label_agreement":null},{"id":"W4223427803","doi":"10.1130/2021.2554(06)","title":"Geochemical and Nd isotopic constraints on the origin of uppermost Silurian rhyolitic rocks in the northern Appalachians (northern New Brunswick): Tectonic implications","year":2022,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":true,"ca_institutions":"University of Fredericton; Saint Mary's University","funders":"","keywords":"Felsic; Geology; Mafic; Geochemistry; Rhyolite; Zircon; Anatexis; Continental crust; Fractional crystallization (geology); Partial melting; Volcanic rock; Crust; Basalt; Petrology; Volcano","score_opus":0.016909505388749812,"score_gpt":0.20180781779193072,"score_spread":0.18489831240318091,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4223427803","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.4367466,0.0011825148,0.00006898632,0.016203357,0.000047563404,0.0010993569,0.00034187266,0.000059572205,0.5442502],"genre_scores_gemma":[0.98923993,0.00018507322,0.00018030818,0.0029447929,0.00008244223,0.000009386617,0.00019298424,0.000007815815,0.0071572564],"study_design_codex":"observational","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99774516,0.0001239144,0.00061791076,0.00059103,0.00045305974,0.00046892115],"domain_scores_gemma":[0.9976606,0.0012347959,0.0004000503,0.00049116503,0.00005917243,0.00015421466],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002839552,0.00039775023,0.0007174157,0.000037926606,0.00025656176,0.000020118248,0.0007971114,0.00030554848,0.012876923],"category_scores_gemma":[0.0000772017,0.00021237099,0.00058169133,0.00011242756,0.0024467295,0.000016485856,0.00011678123,0.0010823667,0.00003506762],"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":[0.00019425135,0.00028609775,0.69875425,0.00016223299,0.0009192709,0.00003074133,0.0032437895,0.00098531,0.00025362993,0.038519517,0.0019304783,0.25472042],"study_design_scores_gemma":[0.001453676,0.0024285545,0.37204102,0.00017390386,0.00074056484,0.0001768024,0.004037715,0.0011446899,0.00009891851,0.46245906,0.15336283,0.0018822533],"about_ca_topic_score_codex":0.010208605,"about_ca_topic_score_gemma":0.004343442,"teacher_disagreement_score":0.55249333,"about_ca_system_score_codex":0.00001627745,"about_ca_system_score_gemma":0.0002106055,"threshold_uncertainty_score":0.9963825},"labels":[],"label_agreement":null},{"id":"W4223531795","doi":"10.1130/2021.2554(08)","title":"Insights from Lu-Hf zircon isotopic data on the crustal evolution of Avalonia and Ganderia in the northern Appalachian orogen","year":2022,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","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":"Nova Scotia Department of Energy; Cape Breton University; Acadia University; Mount Royal University","funders":"","keywords":"Geology; Zircon; Magmatism; Geochemistry; Subduction; Terrane; Metamorphism; Back-arc basin; Continental arc; Petrology; Paleontology; Tectonics","score_opus":0.02323883058140538,"score_gpt":0.1903007343309498,"score_spread":0.1670619037495444,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4223531795","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6894884,0.0032549568,0.000092099384,0.0036420217,0.00008754833,0.0007948066,0.0010814215,0.00004049632,0.30151823],"genre_scores_gemma":[0.9954941,0.0002108687,0.0002788472,0.0012793298,0.00007597449,0.000004364064,0.00067304197,0.0000041158414,0.0019793196],"study_design_codex":"observational","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99807686,0.00017289822,0.00044650864,0.00057683996,0.0004898222,0.00023707532],"domain_scores_gemma":[0.99818695,0.00072983355,0.0003639355,0.0006197989,0.00003399638,0.00006551092],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00021969005,0.00028652028,0.00057346927,0.000025728508,0.00020237008,0.000016592523,0.0009987848,0.00024148401,0.005134421],"category_scores_gemma":[0.000050230927,0.00013819682,0.00027876705,0.00006726628,0.001094937,0.000029480343,0.00026992336,0.0006998915,0.000019481431],"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":[0.0015234044,0.00086748507,0.57345873,0.00040199337,0.0040446455,0.00016178234,0.013323,0.0021947965,0.0023982346,0.077676125,0.008872621,0.3150772],"study_design_scores_gemma":[0.00094706,0.0019759568,0.3139697,0.000103825274,0.00059720344,0.000011953845,0.008390553,0.007669095,0.00006671854,0.5470925,0.118010126,0.0011653173],"about_ca_topic_score_codex":0.011169066,"about_ca_topic_score_gemma":0.0024861859,"teacher_disagreement_score":0.46941638,"about_ca_system_score_codex":0.000009813054,"about_ca_system_score_gemma":0.000040449573,"threshold_uncertainty_score":0.99577504},"labels":[],"label_agreement":null},{"id":"W4223577869","doi":"10.1130/2022.2554(09)","title":"Conditions and timing of metamorphism near the Baie Verte Line (Baie Verte Peninsula, NW Newfoundland, Canada): Multiple reactivations within the suture zone of an arc-continent collision","year":2022,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":"University of Waterloo; Geological Survey of Canada","funders":"","keywords":"Geology; Forearc; Terrane; Subduction; Fibrous joint; Paleontology; Seismology; Oceanic crust; Greenschist; Metamorphism; Collision zone; Petrology; Geochemistry","score_opus":0.017933757538311276,"score_gpt":0.19742060965260014,"score_spread":0.17948685211428886,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4223577869","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9365532,0.0014281448,0.00026954617,0.008872759,0.0002200712,0.0011465097,0.0027442325,0.000054100565,0.04871144],"genre_scores_gemma":[0.9888854,0.0001656447,0.0016505542,0.0012020807,0.000061607,0.000007884517,0.00091690617,0.0000068408303,0.0071030697],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99781436,0.00012535769,0.0006707113,0.00043370517,0.00065712456,0.0002987565],"domain_scores_gemma":[0.99727076,0.0012002282,0.00081006496,0.00039633614,0.00017484624,0.00014778404],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00035693866,0.00031916331,0.00080770697,0.000024915984,0.00074028503,0.000023074579,0.0004968879,0.00020951622,0.004427682],"category_scores_gemma":[0.00012700372,0.00016785655,0.00042963962,0.00011008135,0.0022865194,0.000044391865,0.00016473325,0.0007158305,0.0000022058769],"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":[0.0058533982,0.0022922854,0.4188892,0.0016319526,0.021490071,0.00033642616,0.02426002,0.22047357,0.023465639,0.05409722,0.048193675,0.17901655],"study_design_scores_gemma":[0.0029974766,0.00420925,0.29280812,0.00024014273,0.003523978,0.00008176687,0.006366774,0.26660714,0.001100963,0.06279816,0.35696897,0.0022972552],"about_ca_topic_score_codex":0.37221265,"about_ca_topic_score_gemma":0.08481987,"teacher_disagreement_score":0.3087753,"about_ca_system_score_codex":0.000015795074,"about_ca_system_score_gemma":0.00020577993,"threshold_uncertainty_score":0.99648243},"labels":[],"label_agreement":null},{"id":"W4224219812","doi":"10.1130/mwr220","title":"Laurentia: Turning Points in the Evolution of a Continent","year":2022,"lang":"en","type":"book","venue":"Geological Society of America eBooks","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":"Bedford Institute of Oceanography; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Laurentia; Rodinia; Geology; Supercontinent; Paleontology; Orogeny; Paleozoic; Rift; Paleomagnetism; Earth science; Tectonics; Craton","score_opus":0.01000336362216403,"score_gpt":0.18767398752269043,"score_spread":0.1776706239005264,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4224219812","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.084800996,0.0038194663,0.00026477603,0.0020111266,0.00012617587,0.00058969675,0.0002688757,0.000053913645,0.90806496],"genre_scores_gemma":[0.938914,0.00020202596,0.00189283,0.0019899292,0.00012336783,0.000012600502,0.0005845832,0.00000541385,0.056275275],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99781865,0.00022738309,0.00058781327,0.00039559448,0.0006161807,0.0003543558],"domain_scores_gemma":[0.9984888,0.00060237263,0.00054219394,0.00024638284,0.000059474565,0.000060813694],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00052326964,0.00024661372,0.0007277886,0.000043470704,0.000107782755,0.000008322472,0.0006536788,0.00024129408,0.017314952],"category_scores_gemma":[0.00007775577,0.00014240172,0.00078015804,0.00017791685,0.0009263354,0.00001705793,0.00011594365,0.00081151753,0.000021101912],"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":[0.00068636425,0.0009111045,0.6910834,0.0009409701,0.0018240035,0.000116564755,0.0069213402,0.0067161797,0.00051939633,0.005021858,0.14823753,0.13702132],"study_design_scores_gemma":[0.0011923196,0.002352052,0.285322,0.00016360685,0.0006117484,0.000032126016,0.008208119,0.0067166025,0.000045932557,0.2944996,0.39963865,0.0012172386],"about_ca_topic_score_codex":0.0030221131,"about_ca_topic_score_gemma":0.00015687183,"teacher_disagreement_score":0.854113,"about_ca_system_score_codex":0.000022979295,"about_ca_system_score_gemma":0.00008270844,"threshold_uncertainty_score":0.98358333},"labels":[],"label_agreement":null},{"id":"W4224225948","doi":"10.1130/2022.1220(08)","title":"Laurentia in transition during the Mesoproterozoic: Observations and speculation on the ca. 1500–1340 Ma tectonic evolution of the southern Laurentian margin","year":2022,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical 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":"Memorial University of Newfoundland","funders":"","keywords":"Laurentia; Supercontinent; Rodinia; Baltica; Geology; Paleontology; Tectonics; Magmatism; Ordovician; Earth science; Craton","score_opus":0.013318011905549673,"score_gpt":0.1672236017566916,"score_spread":0.15390558985114192,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4224225948","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9408435,0.000967792,0.000102939295,0.007693641,0.00007526406,0.0010247888,0.00059203047,0.000036357782,0.04866367],"genre_scores_gemma":[0.992422,0.00007435264,0.00010814678,0.00046640474,0.000040218674,0.00001039918,0.00010928346,0.0000042983047,0.006764918],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983589,0.00015125475,0.00039972714,0.00033636528,0.00052407733,0.00022966384],"domain_scores_gemma":[0.9990434,0.00023302989,0.0003526812,0.00028299371,0.000049992934,0.00003787158],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00031901218,0.00022673889,0.0003428339,0.000027269722,0.0003715834,0.000014492264,0.0003625817,0.00018345396,0.012070805],"category_scores_gemma":[0.000028445787,0.00010482107,0.00046920203,0.000117046984,0.0009456002,0.000021723281,0.00008117353,0.0006385715,0.000008629838],"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":[0.0020091045,0.00084377086,0.6711218,0.001529404,0.00420648,0.000036688863,0.02455179,0.09838667,0.0114765,0.09570579,0.0051258937,0.08500613],"study_design_scores_gemma":[0.00057525333,0.00042002433,0.8234177,0.0001655992,0.00036382786,0.00001028199,0.002749526,0.009838659,0.00014591828,0.14618771,0.01554617,0.0005793016],"about_ca_topic_score_codex":0.003669528,"about_ca_topic_score_gemma":0.0013232239,"teacher_disagreement_score":0.15229596,"about_ca_system_score_codex":0.000023916868,"about_ca_system_score_gemma":0.000026952155,"threshold_uncertainty_score":0.9888323},"labels":[],"label_agreement":null},{"id":"W4224250095","doi":"10.1130/2022.1220(03)","title":"The Neoarchean, a turning point for geodynamic and magmatic processes within the Superior craton?","year":2022,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":true,"ca_institutions":"Saint Mary's University; Laurentian University; Université du Québec à Chicoutimi","funders":"","keywords":"Craton; Geology; Archean; Lithosphere; Diachronous; Earth science; Geochemistry; Subduction; Plate tectonics; Mantle (geology); Tectonics; Paleontology","score_opus":0.012710532947104058,"score_gpt":0.19560334497398346,"score_spread":0.1828928120268794,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4224250095","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.17259046,0.027593004,0.0014455207,0.04046017,0.00049879943,0.0058073895,0.0013501631,0.00047413757,0.74978036],"genre_scores_gemma":[0.8067151,0.003013397,0.012301847,0.011489743,0.00039202778,0.00018365042,0.00065173267,0.000042274583,0.16521026],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.998,0.00007280811,0.00054690865,0.00050997053,0.00042824887,0.00044201143],"domain_scores_gemma":[0.9966451,0.0023778302,0.00045376396,0.00027816062,0.00012033143,0.00012480686],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005765819,0.0003636653,0.00062239886,0.000016112892,0.001036604,0.00006864966,0.0005987422,0.00019795008,0.0034176938],"category_scores_gemma":[0.0002479058,0.0001656557,0.00049337436,0.00006276423,0.0025961855,0.00002966911,0.00019306372,0.0007200836,0.000012032736],"study_design_candidate":"design_other","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":[0.0014428307,0.00014255667,0.018192941,0.0028683904,0.004110214,0.00004713326,0.009971639,0.0043414463,0.00052737765,0.050969053,0.009841448,0.897545],"study_design_scores_gemma":[0.00049797917,0.0017150914,0.0038281681,0.00008159517,0.00059143966,0.000057450903,0.0040373616,0.018983424,0.000046218887,0.7518244,0.21739787,0.0009390408],"about_ca_topic_score_codex":0.00065128366,"about_ca_topic_score_gemma":0.00040819118,"teacher_disagreement_score":0.8966059,"about_ca_system_score_codex":0.000007689255,"about_ca_system_score_gemma":0.000084509746,"threshold_uncertainty_score":0.9974933},"labels":[],"label_agreement":null},{"id":"W4224293442","doi":"10.1130/2022.1220(06)","title":"Rapid postorogenic cooling of the Paleoproterozoic Cape Smith foreland thrust belt and footwall Archean basement, Trans-Hudson orogen, Canada","year":2022,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":true,"ca_institutions":"Arcadis (Canada); Bedford Institute of Oceanography; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Hornblende; Metamorphism; Archean; Geochemistry; Craton; Foreland basin; Biotite; Precambrian; Metamorphic facies; Metamorphic rock; Muscovite; Greenschist; Geomorphology; Paleontology; Tectonics; Facies","score_opus":0.014395262680781356,"score_gpt":0.167694767836836,"score_spread":0.15329950515605464,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4224293442","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6077359,0.018983498,0.00011441715,0.0031302436,0.00027236636,0.0018159194,0.002329208,0.00008812988,0.36553034],"genre_scores_gemma":[0.9878792,0.0013857223,0.0007912919,0.0017747872,0.00006631387,0.000008295602,0.0002535638,0.000010849964,0.007829954],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9974363,0.0000972909,0.0006421527,0.0006074977,0.0007052966,0.000511467],"domain_scores_gemma":[0.99844456,0.00034023487,0.0005531687,0.00035597145,0.00008230152,0.0002237704],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00024480894,0.0004390448,0.00090782315,0.000023229892,0.00034262103,0.000010945167,0.0005777312,0.00026846997,0.016420845],"category_scores_gemma":[0.000026341817,0.00026662086,0.0007676663,0.000070421236,0.0013094273,0.000019055295,0.00016124496,0.0007835149,0.0000017563667],"study_design_candidate":"not_applicable","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":[0.0011234842,0.00022440453,0.4319507,0.0014832905,0.005113373,0.00010962021,0.0021901536,0.0014792316,0.00079150253,0.0023649926,0.008102601,0.54506665],"study_design_scores_gemma":[0.0027946066,0.004645802,0.23991919,0.00035212035,0.0026439782,0.00012659449,0.001958754,0.0056874943,0.0012963548,0.044926714,0.6922674,0.0033809629],"about_ca_topic_score_codex":0.21809964,"about_ca_topic_score_gemma":0.082172304,"teacher_disagreement_score":0.6841648,"about_ca_system_score_codex":0.000020807038,"about_ca_system_score_gemma":0.0002209613,"threshold_uncertainty_score":0.9999786},"labels":[],"label_agreement":null},{"id":"W4225852063","doi":"10.1130/2022.2554(03)","title":"Evolving views of West Avalonia: Perspectives from southeastern New England, USA","year":2022,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical 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":"Mount Royal University; Acadia University","funders":"","keywords":"Terrane; Geology; Zircon; Baltica; Volcanic rock; Felsic; Pluton; Transtension; Magmatism; Cape; Geochemistry; Ordovician; Volcano; Paleontology; Rift; Archaeology; Structural basin; Geography; Tectonics","score_opus":0.024217860371245455,"score_gpt":0.2035847166401635,"score_spread":0.17936685626891805,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4225852063","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.03344845,0.007091567,0.00024534427,0.0009165954,0.00013468185,0.00036998512,0.0010277992,0.00007926084,0.9566863],"genre_scores_gemma":[0.8180211,0.0011352936,0.009732654,0.0009929427,0.0005519107,0.000004083107,0.00065924425,0.000017280625,0.16888548],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9972633,0.000093213916,0.0007320318,0.00079796213,0.00067272806,0.00044073886],"domain_scores_gemma":[0.99793077,0.00053597393,0.00074482575,0.00040053332,0.00011275231,0.00027517884],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0001976913,0.00048457427,0.0013507084,0.00004365377,0.00016869328,0.00001784027,0.0006819634,0.00039010972,0.22328342],"category_scores_gemma":[0.000062923464,0.0003395855,0.00136788,0.00006615497,0.0010502775,0.000039565573,0.00022676628,0.0008359344,0.0002832748],"study_design_candidate":"not_applicable","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":[0.0008084811,0.00033637023,0.4187334,0.00028830493,0.004277772,0.0000922507,0.017583914,0.0013865071,0.0010655258,0.0042790477,0.008517357,0.5426311],"study_design_scores_gemma":[0.001976717,0.0028144317,0.105985366,0.00017701897,0.0012549318,0.00002038663,0.0054210806,0.0020462845,0.000116782074,0.23640469,0.6415598,0.0022225091],"about_ca_topic_score_codex":0.01717468,"about_ca_topic_score_gemma":0.0008236298,"teacher_disagreement_score":0.78780085,"about_ca_system_score_codex":0.000009768422,"about_ca_system_score_gemma":0.00007467377,"threshold_uncertainty_score":0.99990565},"labels":[],"label_agreement":null},{"id":"W4226158670","doi":"10.1130/2021.2554(07)","title":"U-Pb zircon ages and Sm-Nd isotopic data from the Cobequid Highlands, Nova Scotia, Canada: New contributions to understanding the Neoproterozoic geologic history of Avalonia","year":2022,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Cape Breton University; Acadia University; Nova Scotia Department of Energy","funders":"","keywords":"Geology; Zircon; Geochemistry; Pluton; Felsic; Volcanic rock; Mafic; Devonian; Igneous rock; Volcano; Paleontology; Tectonics","score_opus":0.054390532827444604,"score_gpt":0.2141738522834551,"score_spread":0.1597833194560105,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4226158670","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.058284257,0.09954445,0.019988393,0.21122117,0.0035544161,0.007675142,0.034887757,0.00043439263,0.56441003],"genre_scores_gemma":[0.8911884,0.0009114914,0.002682587,0.019037616,0.0005503436,0.000007533092,0.0038710583,0.000018159777,0.08173281],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.997493,0.00013134565,0.0005948932,0.0007322518,0.00058804196,0.00046041654],"domain_scores_gemma":[0.99708235,0.0013319904,0.0005207837,0.0007671775,0.00006478755,0.00023290995],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00035729495,0.00038799012,0.0008682827,0.000021916485,0.0002825644,0.000019375902,0.0013629498,0.0002553157,0.021961961],"category_scores_gemma":[0.00014725754,0.00020893305,0.00029431022,0.00006841918,0.001554495,0.000034914687,0.00064853823,0.00078075525,0.000019999503],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00049649714,0.00009267138,0.07517206,0.000151513,0.0031984511,0.00008359626,0.0019623998,0.0013237486,0.0008757992,0.013384477,0.87864137,0.02461744],"study_design_scores_gemma":[0.0008108188,0.0010805369,0.042248163,0.000097396354,0.0010098543,0.000023171366,0.0012003895,0.0012482753,0.000040156337,0.1241588,0.8270262,0.0010562253],"about_ca_topic_score_codex":0.7773085,"about_ca_topic_score_gemma":0.3386193,"teacher_disagreement_score":0.83290416,"about_ca_system_score_codex":0.00012258437,"about_ca_system_score_gemma":0.00046260573,"threshold_uncertainty_score":0.9789321},"labels":[],"label_agreement":null},{"id":"W4229369984","doi":"10.1130/2022.1220(09)","title":"Circa 1.50–1.45 Ga metasedimentary rocks in southwestern Laurentia provide distinctive records of Mesoproterozoic regional orogenesis and craton interactions","year":2022,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","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":"","keywords":"Laurentia; Zircon; Geology; Rodinia; Craton; Orogeny; Supercontinent; Metamorphism; Geochemistry; Paleontology; Ordovician; Tectonics","score_opus":0.019423134747134554,"score_gpt":0.20761073851588305,"score_spread":0.1881876037687485,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4229369984","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.58979464,0.0095853815,0.0011091065,0.004008183,0.0004881075,0.0027978397,0.0041690473,0.0002526928,0.387795],"genre_scores_gemma":[0.9658584,0.0006718796,0.0035184221,0.0020920527,0.00013555975,0.00004489753,0.0018500676,0.000019040168,0.025809688],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99753046,0.000117483345,0.00076132297,0.0007400313,0.0004845326,0.00036617462],"domain_scores_gemma":[0.99838436,0.00042833085,0.00067552907,0.0002546335,0.00007953763,0.00017761464],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00020839937,0.0004205437,0.001017015,0.000087263645,0.00015293433,0.000013271749,0.00033838573,0.00025060502,0.029371448],"category_scores_gemma":[0.000027193946,0.00031765414,0.00070942304,0.00008795318,0.0010821832,0.000060128667,0.00020742134,0.0007159696,0.000013289153],"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":[0.0015466578,0.00059830816,0.66744214,0.0006892282,0.0038650557,0.00010683149,0.0018908773,0.0012962442,0.0009844339,0.00087592495,0.0047681457,0.31593618],"study_design_scores_gemma":[0.0030152742,0.006260268,0.27751163,0.0005580197,0.0033665446,0.00016012003,0.004338973,0.0055123954,0.00094607513,0.17959164,0.5146827,0.004056362],"about_ca_topic_score_codex":0.011881147,"about_ca_topic_score_gemma":0.0016868471,"teacher_disagreement_score":0.5099145,"about_ca_system_score_codex":0.000019579522,"about_ca_system_score_gemma":0.0000507072,"threshold_uncertainty_score":0.9999276},"labels":[],"label_agreement":null},{"id":"W4232833157","doi":"10.1130/spe551","title":"Biostratigraphy, Age, and Paleoenvironment of the Pliocene Beaufort Formation on Meighen Island, Canadian Arctic Archipelago","year":2021,"lang":"en","type":"book","venue":"Geological Society of America eBooks","topic":"Geological Studies and Exploration","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":"Archipelago; Geology; Arctic; Neogene; Paleontology; Bay; Oceanography; Paleomagnetism; Ecological succession; Beaufort scale; Sea level; Structural basin; Ecology","score_opus":0.016572105033069252,"score_gpt":0.17702934015076627,"score_spread":0.16045723511769702,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4232833157","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.15379584,0.0042522694,0.0002551332,0.004383072,0.00049930386,0.0021385793,0.0014716472,0.000049448583,0.8331547],"genre_scores_gemma":[0.9855178,0.0014958178,0.0007942623,0.002314659,0.000068374226,0.000006188615,0.00061185565,0.0000042609818,0.009186755],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.998603,0.00007382466,0.00036599266,0.0003012157,0.00033849763,0.00031746956],"domain_scores_gemma":[0.99910694,0.00019016581,0.00030465878,0.0002141899,0.00004496587,0.00013908879],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012306383,0.00024053101,0.00044926564,0.000025565989,0.0002518863,0.000015951444,0.00020981286,0.00025331645,0.0005764829],"category_scores_gemma":[0.00003484694,0.00014152353,0.00032343648,0.000057981146,0.0010257455,0.000023352568,0.000050802413,0.00033787184,0.000008050997],"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":[0.00022073681,0.00019795782,0.20480734,0.0011719073,0.0013130163,0.00007708502,0.009335366,0.0032211833,0.000064197324,0.0022723624,0.059906367,0.7174125],"study_design_scores_gemma":[0.00043672486,0.0015941117,0.86620086,0.00021892795,0.0001606895,0.000010671636,0.0018816794,0.0005976769,0.000050339255,0.021264004,0.10704513,0.00053915376],"about_ca_topic_score_codex":0.0195154,"about_ca_topic_score_gemma":0.03291288,"teacher_disagreement_score":0.83172196,"about_ca_system_score_codex":0.000017974007,"about_ca_system_score_gemma":0.000060822826,"threshold_uncertainty_score":0.98701376},"labels":[],"label_agreement":null},{"id":"W4241223050","doi":"10.1130/dnag-gna-p1.33","title":"Stratiform Phosphate","year":2015,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Mineralogy and Gemology 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":"","keywords":"Mineral; Section (typography); Volume (thermodynamics); Government (linguistics); Mineral deposit; Mineralogy; Geology; Computer science; Business; Geochemistry; Metallurgy; Materials science; Linguistics; Philosophy; Advertising","score_opus":0.041059640590446964,"score_gpt":0.22693364298564794,"score_spread":0.18587400239520097,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4241223050","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00030881548,0.0034783855,0.00007893806,0.00033869062,0.0001685372,0.0001695389,0.00013876811,0.000059590842,0.99525875],"genre_scores_gemma":[0.027095154,0.0008168463,0.0046400563,0.0031439962,0.00025583574,0.0000022530262,0.00026524052,0.000009663134,0.9637709],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99860144,0.000021260958,0.0003643232,0.00038533573,0.00027409976,0.00035356457],"domain_scores_gemma":[0.9990573,0.00015612094,0.00031767567,0.00022434059,0.00010711566,0.00013743145],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00019662562,0.00033029765,0.0006900973,0.00001851015,0.00014565006,0.0000069183875,0.0002855729,0.00055090437,0.0081290165],"category_scores_gemma":[0.00001579812,0.00023432872,0.00038214886,0.000014858528,0.0020577349,0.000024002285,0.000055719804,0.00048880244,0.00039713425],"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":[0.00023490051,0.000032516313,0.013964753,0.00012795744,0.0013709499,0.000075525124,0.0011863874,0.00028727597,0.0000054605434,0.01882801,0.4152221,0.54866415],"study_design_scores_gemma":[0.0002903417,0.00087549794,0.0042999024,0.000026756697,0.00010698429,0.000018472767,0.00020511032,0.0001808176,0.000005252689,0.10739895,0.8861249,0.0004670176],"about_ca_topic_score_codex":0.00042054272,"about_ca_topic_score_gemma":0.000073983225,"teacher_disagreement_score":0.54819715,"about_ca_system_score_codex":0.0000050490207,"about_ca_system_score_gemma":0.000066521396,"threshold_uncertainty_score":0.9927777},"labels":[],"label_agreement":null},{"id":"W4247265349","doi":"10.1130/2020.0058(01)","title":"Architecture and Evolution of the Crust during Continental Arc Magmatism: A Transect through the Coast Mountains Batholith, British Columbia","year":2020,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Batholith; Pluton; Paleogene; Gneiss; Shear zone; Metamorphic rock; Cretaceous; Geochemistry; Continental crust; Paleontology; Crust; Geomorphology; Tectonics","score_opus":0.007636083540492033,"score_gpt":0.16336981740945752,"score_spread":0.1557337338689655,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4247265349","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.80624133,0.0035153665,0.0005490651,0.0036478124,0.00010023607,0.0010385766,0.0017305536,0.00009773479,0.18307935],"genre_scores_gemma":[0.9851071,0.00025228385,0.0008418331,0.0010145481,0.00008711671,0.000003469756,0.000050290913,0.0000061161395,0.012637219],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99815273,0.00009095187,0.0004986942,0.00048223662,0.0004480515,0.0003273414],"domain_scores_gemma":[0.99895066,0.00023420536,0.00041324063,0.00022874163,0.000067697845,0.00010546714],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000100583835,0.00026684755,0.00073573116,0.000006626028,0.00035965611,0.000054594144,0.00046629098,0.00030709928,0.0029591492],"category_scores_gemma":[0.00004080032,0.00018033289,0.000815159,0.0000705112,0.0032256255,0.000024025423,0.00014408224,0.00077414536,0.00000549494],"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":[0.00087372167,0.00033077327,0.67758185,0.002783172,0.004443417,0.00017536155,0.012546123,0.0029137488,0.005040456,0.0049581532,0.015581137,0.27277207],"study_design_scores_gemma":[0.00096005027,0.0006854829,0.75488,0.0003109927,0.00067523425,0.00025814126,0.0017906327,0.001031176,0.00008206103,0.2173075,0.021155935,0.0008628011],"about_ca_topic_score_codex":0.048105475,"about_ca_topic_score_gemma":0.016127348,"teacher_disagreement_score":0.2719093,"about_ca_system_score_codex":0.00000872183,"about_ca_system_score_gemma":0.00003321074,"threshold_uncertainty_score":0.99948704},"labels":[],"label_agreement":null},{"id":"W4256075051","doi":"10.1130/fld048","title":"Geologic Field Trips of the Canadian Rockies: 2017 Meeting of the GSA Rocky Mountain Section","year":2017,"lang":"en","type":"book","venue":"Geological Society of America eBooks","topic":"Geological Modeling and Analysis","field":"Earth and Planetary Sciences","cited_by":2,"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":"Section (typography); TRIPS architecture; Field trip; Field (mathematics); Geology; Geography; Engineering; Political science; Transport engineering; Advertising; Business; Law","score_opus":0.023536238208220747,"score_gpt":0.21156036924869148,"score_spread":0.18802413104047072,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4256075051","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.03561575,0.0014114083,0.00032575591,0.002662173,0.0007010719,0.0006775537,0.00029661172,0.00004753758,0.95826215],"genre_scores_gemma":[0.87768817,0.00017537925,0.00039732605,0.0011319532,0.00019442137,0.0000028274405,0.000039488707,0.0000047625335,0.12036564],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9976069,0.0002256588,0.00065938616,0.00045560242,0.00055828533,0.0004941803],"domain_scores_gemma":[0.9969226,0.00046573087,0.0014718758,0.00078840344,0.00021289701,0.00013846389],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000570593,0.0003328343,0.000884505,0.000042483633,0.0009389316,0.000025594069,0.001558778,0.00085413054,0.0007277202],"category_scores_gemma":[0.0004682631,0.00016895814,0.0012873791,0.00008956193,0.0015044807,0.000027279593,0.00017401548,0.0009301606,0.000010344543],"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":[0.00022875363,0.00013909831,0.5407454,0.0008703536,0.0020799306,0.000013795817,0.0032011354,0.120907746,0.0001436497,0.0004888826,0.16507198,0.1661093],"study_design_scores_gemma":[0.0015255666,0.003043706,0.25297517,0.0015936015,0.0020581088,0.00005703947,0.0034550857,0.07427856,0.0007827185,0.097732805,0.5598759,0.002621737],"about_ca_topic_score_codex":0.27734116,"about_ca_topic_score_gemma":0.07473857,"teacher_disagreement_score":0.8420724,"about_ca_system_score_codex":0.000030749663,"about_ca_system_score_gemma":0.0004997112,"threshold_uncertainty_score":0.94214505},"labels":[],"label_agreement":null},{"id":"W4283705308","doi":"10.1130/2022.2554(001)","title":"Introduction","year":2022,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"St. Francis Xavier University","funders":"","keywords":"Geography","score_opus":0.01279331013478108,"score_gpt":0.1785545910952687,"score_spread":0.16576128096048762,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4283705308","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0010047999,0.00061800197,0.00006325923,0.002386332,0.00014043701,0.00014586681,0.00012877592,0.000092742615,0.9954198],"genre_scores_gemma":[0.061539173,0.0011625029,0.008081833,0.00524245,0.0015319758,0.000007201498,0.0017399321,0.00001588239,0.92067903],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9980626,0.000038167953,0.00044611428,0.000610765,0.0004952712,0.00034704787],"domain_scores_gemma":[0.9989418,0.00016835214,0.00037630834,0.00029975662,0.000066747176,0.00014705164],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00016166775,0.0003209579,0.0006944023,0.000031990672,0.00019562365,0.000010860268,0.00038665548,0.0002916282,0.3582406],"category_scores_gemma":[0.000027289501,0.00023110039,0.0009201959,0.00005049174,0.0009992023,0.000024466915,0.00012022683,0.00073540624,0.0003595835],"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":[0.00025604005,0.000103712104,0.009676357,0.00016974045,0.0013251408,0.000040981613,0.00029067977,0.0022103102,0.00019828172,0.031110989,0.15825559,0.79636216],"study_design_scores_gemma":[0.00008567907,0.00040738547,0.0013874846,0.000003941363,0.00010631353,0.000008452988,0.0000607629,0.00036749858,0.000018964029,0.0914214,0.90581965,0.00031245482],"about_ca_topic_score_codex":0.0007926482,"about_ca_topic_score_gemma":0.000017730208,"teacher_disagreement_score":0.7960497,"about_ca_system_score_codex":0.000009152771,"about_ca_system_score_gemma":0.00002486858,"threshold_uncertainty_score":0.9424001},"labels":[],"label_agreement":null},{"id":"W4283710792","doi":"10.1130/2021.2554(001)","title":"Paleozoic orogenies and relative plate motions at the sutures of the Iapetus-Rheic Ocean","year":2022,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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 Calgary","funders":"","keywords":"Gondwana; Geology; Laurentia; Paleontology; Plate tectonics; Paleozoic; Ordovician; Subduction; Craton; Supercontinent; Passive margin; Seafloor spreading; Rift; Convergent boundary; Continental margin; Oceanic crust; Tectonics","score_opus":0.013502295053183297,"score_gpt":0.1800124162054181,"score_spread":0.16651012115223482,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4283710792","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.22978872,0.008363897,0.000022169728,0.005334538,0.00014789564,0.0006697694,0.00096958445,0.000072259114,0.75463116],"genre_scores_gemma":[0.8504236,0.0016969034,0.0005051252,0.0019522617,0.000074601565,0.0000037020486,0.00018531957,0.000007919351,0.14515059],"study_design_codex":"observational","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99822605,0.000113706505,0.00044580805,0.00043901626,0.00047167626,0.00030371879],"domain_scores_gemma":[0.9981751,0.00078961934,0.0005331033,0.00034191125,0.00006439246,0.0000958859],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00019804781,0.00031557158,0.0006121852,0.000017429993,0.00060385786,0.000010123834,0.00051469257,0.00025505997,0.024273513],"category_scores_gemma":[0.00006913996,0.00014484064,0.0009594661,0.00007447824,0.003884733,0.00002303612,0.00040237262,0.00071984,0.000019748026],"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":[0.00072328077,0.0003207915,0.6320489,0.00060719106,0.010713614,0.000056497276,0.011228149,0.010353598,0.00075611327,0.10401517,0.041822065,0.18735461],"study_design_scores_gemma":[0.00051502686,0.0011510954,0.19738722,0.000073951975,0.0012435248,0.00005771257,0.0014544736,0.0011156987,0.00019535937,0.40456533,0.39121833,0.0010222753],"about_ca_topic_score_codex":0.0007931157,"about_ca_topic_score_gemma":0.00019008006,"teacher_disagreement_score":0.62063485,"about_ca_system_score_codex":0.0000078618095,"about_ca_system_score_gemma":0.000026225502,"threshold_uncertainty_score":0.99882615},"labels":[],"label_agreement":null},{"id":"W4283767500","doi":"10.1130/2022.1220(02)","title":"Sedimentary processes, provenance, and tectonic control on fluvial sandstone geochemistry during Superior craton stabilization","year":2022,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":false,"ca_institutions":"Saint Mary's University; Université du Québec à Chicoutimi; Laurentian University","funders":"","keywords":"Geology; Provenance; Craton; Sedimentary rock; Geochemistry; Terrigenous sediment; Sedimentary depositional environment; Tectonics; Fluvial; Archean; Continental margin; Geomorphology; Petrology; Paleontology; Structural basin","score_opus":0.006457161955236255,"score_gpt":0.17189229225203942,"score_spread":0.16543513029680315,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4283767500","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.59751356,0.0033233583,0.000033686334,0.0008955854,0.00009275231,0.000947983,0.00090245187,0.00019921939,0.3960914],"genre_scores_gemma":[0.983735,0.00077510683,0.0003278567,0.0014586223,0.00013716279,0.000018303741,0.00060742284,0.000011072417,0.012929418],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9977131,0.00003897767,0.00049847615,0.00078485045,0.00052807387,0.0004365212],"domain_scores_gemma":[0.9989426,0.0002647055,0.00027797587,0.00023644604,0.000090649366,0.00018762123],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00013110654,0.00044511803,0.0008096535,0.00003240197,0.0003358768,0.000021638432,0.00027352016,0.00033032612,0.026059654],"category_scores_gemma":[0.000050196875,0.0003288295,0.00036609935,0.000072720366,0.001020521,0.000042021667,0.00010033949,0.0006957761,0.000017414166],"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":[0.013335985,0.002136328,0.48161587,0.014255624,0.009169949,0.000635755,0.0050357473,0.013061808,0.059551287,0.004394508,0.010118188,0.38668895],"study_design_scores_gemma":[0.019027326,0.02170577,0.12975891,0.0013948589,0.0043955264,0.00036840627,0.0040230392,0.012966889,0.035340175,0.14229459,0.61585474,0.0128698],"about_ca_topic_score_codex":0.0005468944,"about_ca_topic_score_gemma":0.000030117271,"teacher_disagreement_score":0.60573655,"about_ca_system_score_codex":0.000021358785,"about_ca_system_score_gemma":0.00007988743,"threshold_uncertainty_score":0.9999164},"labels":[],"label_agreement":null},{"id":"W4285490038","doi":"10.1130/2022.1220(17)","title":"Geon 14 to early Geon 13 granitoid magmatism in the Grenville Province of Canada, northeastern Laurentia: Distribution, geochemical patterns, and links with an active-margin setting","year":2022,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","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":"Ministère des Ressources naturelles et des Forêts (Québec); Memorial University of Newfoundland","funders":"","keywords":"Geology; Geochemistry; Magmatism; Back-arc basin; Plutonism; Laurentia; Continental crust; Pluton; Island arc; Crust; Petrology; Subduction; Paleontology; Ordovician; Tectonics","score_opus":0.005529697441963748,"score_gpt":0.16415106960619275,"score_spread":0.158621372164229,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4285490038","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97742593,0.0002621852,0.00013813586,0.0018557734,0.000029439048,0.0005734596,0.0016967921,0.000021166115,0.0179971],"genre_scores_gemma":[0.9945862,0.00006252421,0.000507962,0.0009903986,0.000054984685,0.000011872677,0.0012548002,0.0000074564327,0.0025237727],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99743605,0.00012408335,0.00053075753,0.00064689247,0.00075472187,0.000507472],"domain_scores_gemma":[0.9986535,0.00030860948,0.0004237772,0.000305213,0.000097347474,0.00021158926],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00026973852,0.00039264828,0.0007311215,0.000026237161,0.00020996275,0.000021759284,0.00053150323,0.00031684688,0.0023776917],"category_scores_gemma":[0.000029533145,0.0002404869,0.00020889968,0.000079648074,0.0006134681,0.000039228416,0.0001527656,0.0011129571,0.0000023075654],"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":[0.00087869976,0.0002218601,0.71184754,0.00045492523,0.0005692384,0.0001828627,0.0019424306,0.0013444407,0.00013372491,0.0005795663,0.0015188459,0.28032586],"study_design_scores_gemma":[0.00082173117,0.0028454452,0.9448666,0.00021010064,0.00029675328,0.00005042352,0.0017593617,0.0016430387,0.00015183883,0.0074192933,0.038692236,0.0012431795],"about_ca_topic_score_codex":0.30761033,"about_ca_topic_score_gemma":0.34785277,"teacher_disagreement_score":0.27908266,"about_ca_system_score_codex":0.000020931891,"about_ca_system_score_gemma":0.000118176395,"threshold_uncertainty_score":0.99853426},"labels":[],"label_agreement":null},{"id":"W4293057189","doi":"10.1130/2022.1220(24)","title":"Paleozoic tectonic evolution of the rifted margins of Laurentia","year":2022,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University; University of Waterloo; Geological Survey of Canada","funders":"","keywords":"Laurentia; Baltica; Gondwana; Geology; Paleontology; Terrane; Paleozoic; Devonian; Orogeny; Subduction; Rift; Passive margin; Ordovician; Tectonics","score_opus":0.010224797271386792,"score_gpt":0.17309308263378492,"score_spread":0.16286828536239814,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4293057189","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.09091111,0.003663486,0.00011347461,0.0005747129,0.00017838359,0.00051869836,0.00078271626,0.000059074697,0.90319836],"genre_scores_gemma":[0.96973634,0.00019927254,0.00082317536,0.00024234303,0.000040204406,0.0000026200682,0.00013948107,0.000004893676,0.028811647],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9979022,0.000085311265,0.00065199414,0.00041346395,0.00063433347,0.00031266393],"domain_scores_gemma":[0.99824333,0.000263362,0.0008896505,0.00040505626,0.00011390541,0.000084707695],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00019268213,0.00029237193,0.0008476599,0.000036173667,0.00015338144,0.000003455357,0.00069934013,0.00032302993,0.05066303],"category_scores_gemma":[0.000042874974,0.0001717983,0.0014455657,0.00013071594,0.0020038106,0.000016266531,0.00021133176,0.00062701036,0.000018345501],"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":[0.0009318074,0.0006963452,0.6900217,0.0016293749,0.005507534,0.00002203496,0.0014939309,0.008318886,0.006600157,0.04905972,0.012244389,0.22347413],"study_design_scores_gemma":[0.0009967721,0.0026442374,0.48436448,0.00019145678,0.0014704879,0.000018039796,0.0007143345,0.003082595,0.00086345547,0.2882598,0.2160578,0.0013365219],"about_ca_topic_score_codex":0.0024001922,"about_ca_topic_score_gemma":0.00013597817,"teacher_disagreement_score":0.87882525,"about_ca_system_score_codex":0.000012149059,"about_ca_system_score_gemma":0.00006708127,"threshold_uncertainty_score":0.9502048},"labels":[],"label_agreement":null},{"id":"W4293057198","doi":"10.1130/2022.1220(05)","title":"Paleoproterozoic geology of SW Montana: Implications for the paleogeography of the Wyoming craton and for the consolidation of Laurentia","year":2022,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","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":"Amherst College; University of Montana","keywords":"Craton; Geology; Supercontinent; Orogeny; Laurentia; Metamorphism; Precambrian; Geochemistry; Rodinia; Terrane; Archean; Rift; Paleontology; Petrology; Tectonics; Ordovician","score_opus":0.021914931547392526,"score_gpt":0.21408938780805298,"score_spread":0.19217445626066046,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4293057198","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.55486494,0.082705185,0.037507854,0.07165173,0.001334869,0.028994823,0.019901728,0.00022479787,0.2028141],"genre_scores_gemma":[0.9952004,0.0008361741,0.0016388368,0.00053369417,0.000045661654,0.000070761576,0.00014703156,0.0000046258438,0.0015228284],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99861634,0.00005177693,0.0005938124,0.0003111522,0.00020145056,0.00022549504],"domain_scores_gemma":[0.99605167,0.0023730157,0.0009791622,0.00036745676,0.00018890733,0.000039815364],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00032550585,0.00020739947,0.00060395553,0.000024095374,0.0003320863,0.000005169262,0.0005696552,0.00020036142,0.0013382792],"category_scores_gemma":[0.000083391555,0.00009538817,0.000996326,0.000078577265,0.0028011524,0.000013754198,0.00013017688,0.00025428782,2.822286e-7],"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":[0.0007527298,0.00017973164,0.55497694,0.00096852385,0.0045137387,3.4038766e-7,0.0013655109,0.0025963334,0.0029312521,0.047621388,0.002770132,0.38132337],"study_design_scores_gemma":[0.0010908352,0.0021931245,0.55613947,0.00007184004,0.00260835,0.000009984838,0.001485559,0.0052861427,0.0010018358,0.33432186,0.09518675,0.0006042358],"about_ca_topic_score_codex":0.0010517144,"about_ca_topic_score_gemma":0.0003074553,"teacher_disagreement_score":0.44033545,"about_ca_system_score_codex":0.0000019218483,"about_ca_system_score_gemma":0.000028846796,"threshold_uncertainty_score":0.9999127},"labels":[],"label_agreement":null},{"id":"W4295920609","doi":"10.1130/2022.1220(11)","title":"Linking the Pinware, Baraboo, and Picuris orogens: Recognition of a trans-Laurentian ca. 1520–1340 Ma orogenic belt","year":2022,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":true,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Zircon; Metamorphism; Geology; Diachronous; Laurentia; Geochemistry; Magmatism; Orogeny; Rodinia; Baltica; Paleontology; Ordovician; Tectonics","score_opus":0.01925345398721514,"score_gpt":0.18837289564206927,"score_spread":0.16911944165485412,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4295920609","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.19324765,0.022255186,0.00035061326,0.0035509593,0.00029105003,0.0016910445,0.0032086233,0.00024393488,0.77516097],"genre_scores_gemma":[0.96437687,0.006802192,0.0037974773,0.0042717075,0.00023787728,0.000021007334,0.002375256,0.000022767965,0.018094838],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9974296,0.00011753605,0.0007312876,0.00066336285,0.00060375745,0.00045444124],"domain_scores_gemma":[0.9983313,0.0004874243,0.0005693507,0.00031305142,0.00012298273,0.00017587078],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00032703244,0.0004380869,0.000947632,0.00004477406,0.00035420756,0.000020283116,0.0004979504,0.00042916683,0.049099527],"category_scores_gemma":[0.000030766903,0.0002744283,0.0010964255,0.000100857986,0.0018333191,0.000035522804,0.00014057456,0.00085124746,0.000029304443],"study_design_candidate":"design_other","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":[0.00042587492,0.00018107198,0.025378114,0.00066339487,0.003005042,0.00005412841,0.003370045,0.0003958435,0.00040007907,0.0012765708,0.0035044341,0.9613454],"study_design_scores_gemma":[0.0014621434,0.0034649768,0.02041247,0.00031161183,0.003069962,0.00012643135,0.0026807778,0.0030394075,0.00040237806,0.3315875,0.6310715,0.002370833],"about_ca_topic_score_codex":0.0024866026,"about_ca_topic_score_gemma":0.0002511477,"teacher_disagreement_score":0.95897454,"about_ca_system_score_codex":0.000008751347,"about_ca_system_score_gemma":0.000047436322,"threshold_uncertainty_score":0.9999708},"labels":[],"label_agreement":null},{"id":"W4296078971","doi":"10.1130/2022.0064(02)","title":"Exploring the nature and extent of the Mesoproterozoic Picuris orogeny in Colorado, USA","year":2022,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical 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":"","keywords":"Orogeny; Laurentia; Geology; Metamorphism; Paleontology; Rift; Mountain formation; Earth science; Geochemistry; Tectonics","score_opus":0.030002104532895823,"score_gpt":0.1952449048260745,"score_spread":0.1652428002931787,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4296078971","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7460705,0.0041738963,0.0000062091485,0.003165038,0.00018167193,0.00080154935,0.00018282614,0.000029214954,0.2453891],"genre_scores_gemma":[0.9854779,0.0012095827,0.00039671396,0.0018228499,0.00005310818,0.000017255416,0.00002795702,0.0000046985374,0.010989881],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99816465,0.00009913138,0.00046969843,0.0004446908,0.00050618197,0.00031564213],"domain_scores_gemma":[0.9987433,0.00040471603,0.0003946964,0.00033327323,0.000044845445,0.00007916989],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00028206038,0.00028857714,0.0006431241,0.000024252358,0.00020775269,0.000010337326,0.0006451767,0.0002536161,0.0087034125],"category_scores_gemma":[0.00004516268,0.00013622221,0.0006112131,0.000100636906,0.0016390833,0.00002925779,0.00033986365,0.0013044921,0.0000072366097],"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":[0.0004643921,0.00021821343,0.5215249,0.0005025055,0.001486019,0.00006217615,0.0032383606,0.0024124547,0.000492735,0.02062934,0.0025334547,0.44643545],"study_design_scores_gemma":[0.0005407342,0.0010508017,0.62685037,0.00012325804,0.0003538736,0.000030083416,0.0011758127,0.0010309181,0.00032899404,0.11445159,0.2531867,0.00087685673],"about_ca_topic_score_codex":0.0021266108,"about_ca_topic_score_gemma":0.00025187284,"teacher_disagreement_score":0.4455586,"about_ca_system_score_codex":0.000008424467,"about_ca_system_score_gemma":0.000026751899,"threshold_uncertainty_score":0.99220276},"labels":[],"label_agreement":null},{"id":"W4303453283","doi":"10.1130/2022.1220(28)","title":"Transformation of eastern North America from compression to extension in the Permian–Triassic","year":2022,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":"Laurentian University","funders":"","keywords":"Geology; Laurentia; Orogeny; Paleontology; Rift; Passive margin; Metamorphism; Tectonics","score_opus":0.024110658205727952,"score_gpt":0.20253128352744681,"score_spread":0.17842062532171887,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4303453283","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.50866324,0.00096263277,0.00068327674,0.0029592395,0.00012353451,0.0010407352,0.0010003038,0.000065566404,0.48450148],"genre_scores_gemma":[0.98670954,0.00033677524,0.0017784977,0.004266377,0.00007596381,0.0000089881405,0.0013448788,0.0000060573625,0.005472918],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9976771,0.00013590038,0.0006946896,0.0004746759,0.000706191,0.00031148084],"domain_scores_gemma":[0.9985533,0.0004961198,0.00043955902,0.0003269288,0.00006492992,0.00011916829],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00017324457,0.00031533968,0.0008320101,0.000053475997,0.00013061381,0.000011136076,0.0006391599,0.00020911095,0.016947286],"category_scores_gemma":[0.000025251704,0.00018248228,0.0006533243,0.00013286139,0.00057514827,0.00003592222,0.00009828777,0.00063238596,0.00008255011],"study_design_candidate":"design_other","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":[0.0006749712,0.00020120088,0.032189477,0.00012296841,0.00029770145,0.000033180204,0.009145319,0.010344362,0.00038598347,0.00030472947,0.0026757307,0.9436244],"study_design_scores_gemma":[0.0014356407,0.0039845826,0.30487075,0.00026905286,0.0005803511,0.000010132275,0.0059053814,0.02433422,0.00010752162,0.049223732,0.60751307,0.0017655441],"about_ca_topic_score_codex":0.006941495,"about_ca_topic_score_gemma":0.0002643382,"teacher_disagreement_score":0.9418588,"about_ca_system_score_codex":0.000008042932,"about_ca_system_score_gemma":0.000023321929,"threshold_uncertainty_score":0.99967134},"labels":[],"label_agreement":null},{"id":"W4307002297","doi":"10.1130/2022.1220(18)","title":"Local rapid exhumation during the long-lived Grenville orogeny","year":2022,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":true,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Metamorphism; Geochemistry; Metamorphic rock; Eclogite; Amphibole; Mafic; Metamorphic facies; Felsic; Granulite; Glaucophane; Orogeny; Petrology; Geomorphology; Facies; Paleontology; Tectonics; Quartz; Subduction","score_opus":0.016144133573047476,"score_gpt":0.18231118539158872,"score_spread":0.16616705181854124,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4307002297","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.046763,0.0027580769,0.00038399687,0.0011666645,0.0001218634,0.00047892242,0.00018240481,0.00012598516,0.9480191],"genre_scores_gemma":[0.91762197,0.0010338795,0.00068226695,0.0019903476,0.00015550797,0.000010464832,0.00042820672,0.000010867893,0.078066476],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9975596,0.00009388135,0.0005774757,0.0006120696,0.00067562336,0.0004813187],"domain_scores_gemma":[0.99851173,0.00035537794,0.00049725675,0.0003957319,0.000075645075,0.00016425326],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000240554,0.00041504257,0.00072840054,0.000030205812,0.0005501504,0.000022105036,0.00067516585,0.0003325182,0.21603301],"category_scores_gemma":[0.000025215531,0.00024334104,0.0011129451,0.000069229776,0.0019754446,0.00002519393,0.00023470719,0.0008659966,0.00024884145],"study_design_candidate":"design_other","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":[0.0005684698,0.00017344671,0.028260624,0.0004336226,0.0026787666,0.00014236326,0.00150994,0.010128813,0.00034724383,0.004159306,0.0063150288,0.9452824],"study_design_scores_gemma":[0.0014976243,0.002465101,0.18158548,0.00010760968,0.0010913142,0.0001392411,0.0023377964,0.009906018,0.0004843066,0.10488251,0.69249797,0.003005],"about_ca_topic_score_codex":0.0010383832,"about_ca_topic_score_gemma":0.000054083444,"teacher_disagreement_score":0.9422774,"about_ca_system_score_codex":0.00001852011,"about_ca_system_score_gemma":0.00003115473,"threshold_uncertainty_score":0.99231595},"labels":[],"label_agreement":null},{"id":"W4307002302","doi":"10.1130/2022.1220(27)","title":"Formation of the Green Mountain anticlinorium in northern Vermont at ca. 420 Ma","year":2022,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical 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":"","keywords":"Orogeny; Geology; Laurentia; Metamorphism; Greenschist; Devonian; Paleozoic; Schist; Paleontology; Ordovician; Plateau (mathematics); Mountain formation; Metamorphic rock; Geochemistry; Geomorphology; Tectonics","score_opus":0.013089880169846212,"score_gpt":0.17949130134972413,"score_spread":0.1664014211798779,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4307002302","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.4789231,0.0007343137,0.000025035852,0.0017894356,0.00009594212,0.0005121938,0.00040945332,0.000036614925,0.5174739],"genre_scores_gemma":[0.9476598,0.00019357966,0.00031024183,0.0011958114,0.000053263815,0.0000041167223,0.0003145627,0.0000052349424,0.0502634],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998051,0.00007752807,0.0006327288,0.00036189696,0.00054817187,0.00032868073],"domain_scores_gemma":[0.9987457,0.00022480488,0.00057785446,0.0003010908,0.00006916991,0.00008142017],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00021434412,0.00027299303,0.0006670142,0.000029346447,0.0001511604,0.0000050033814,0.00054306805,0.00027118446,0.013288975],"category_scores_gemma":[0.000025239182,0.00016255843,0.00077667466,0.0000843509,0.00089265924,0.000030503601,0.00027330013,0.00053069706,0.0000575873],"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":[0.00036434294,0.00011723717,0.9104137,0.00031922208,0.00035211447,0.000028914628,0.0014069135,0.0045128893,0.0005179345,0.0013333671,0.0017801664,0.07885318],"study_design_scores_gemma":[0.0012942036,0.0017020947,0.526325,0.0001282912,0.000509586,0.00003865604,0.0008885276,0.016828934,0.0005939776,0.15756167,0.29249245,0.0016365988],"about_ca_topic_score_codex":0.013659346,"about_ca_topic_score_gemma":0.006419264,"teacher_disagreement_score":0.46873668,"about_ca_system_score_codex":0.00003076558,"about_ca_system_score_gemma":0.000029096194,"threshold_uncertainty_score":0.9929088},"labels":[],"label_agreement":null},{"id":"W4312387718","doi":"10.1130/2022.1220(30)","title":"Paleozoic evolution of the northern Laurentian margin: Evaluating links between the Caledonian, Ellesmerian, and Cordilleran orogens","year":2022,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":true,"ca_institutions":"Yukon University","funders":"","keywords":"Laurentia; Geology; Paleontology; Orogeny; Terrane; Paleozoic; Devonian; Sinistral and dextral; Transpression; Baltica; Passive margin; Ordovician; Structural basin; Tectonics; Rift","score_opus":0.020707341488632177,"score_gpt":0.2088135692958321,"score_spread":0.18810622780719993,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4312387718","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.55341256,0.011733945,0.00026391353,0.018013673,0.000421905,0.0021773481,0.0016658028,0.00016293551,0.4121479],"genre_scores_gemma":[0.98143834,0.00034291777,0.00072439027,0.0014151593,0.00019793333,0.000007334364,0.00021062119,0.000011001261,0.01565233],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9974827,0.0002045507,0.00065186014,0.0005383581,0.0007257059,0.00039679237],"domain_scores_gemma":[0.9979224,0.00063353725,0.0007582348,0.00042912303,0.00013015175,0.00012650527],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00047618715,0.00037015064,0.0007973284,0.000023634475,0.00055615173,0.00001410234,0.0006848005,0.00045493626,0.014012523],"category_scores_gemma":[0.000060444083,0.00018943351,0.00094016956,0.000107647444,0.0025999781,0.000017789356,0.00029495455,0.0012233519,0.000017155844],"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":[0.00009029047,0.000035650253,0.7844797,0.00015035438,0.0012084167,0.0000039584465,0.00064161554,0.0010836008,0.000113442016,0.00083095254,0.0013372594,0.2100248],"study_design_scores_gemma":[0.00085540116,0.0017367622,0.62476736,0.00014455483,0.0019761447,0.000023622206,0.001466012,0.0047672014,0.000051859337,0.10119958,0.26174158,0.0012699013],"about_ca_topic_score_codex":0.0028751986,"about_ca_topic_score_gemma":0.00093716715,"teacher_disagreement_score":0.42802575,"about_ca_system_score_codex":0.0000147379515,"about_ca_system_score_gemma":0.0000732821,"threshold_uncertainty_score":0.9868888},"labels":[],"label_agreement":null},{"id":"W4312436186","doi":"10.1130/2022.1220(001)","title":"The tectonic evolution of Laurentia and the North American continent: New datasets, insights, and models","year":2022,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":"Government of Canada; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Laurentia; Rodinia; Geology; Orogeny; Paleontology; Terrane; Gondwana; Paleozoic; Baltica; Earth science; Rift; Ordovician; Tectonics","score_opus":0.010028909894987451,"score_gpt":0.1721976819060621,"score_spread":0.16216877201107466,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4312436186","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.22935891,0.15653679,0.0021174296,0.017340431,0.00033791762,0.0034964255,0.0051309015,0.00029251914,0.58538866],"genre_scores_gemma":[0.9720048,0.011729602,0.0010030293,0.0010375027,0.00008908557,0.000006531043,0.0008205931,0.000007983882,0.013300914],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9982867,0.000099983845,0.00047337505,0.00044114725,0.00040712708,0.00029162792],"domain_scores_gemma":[0.9981032,0.0007663527,0.00061938557,0.00032248878,0.000048359798,0.00014021316],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00020831006,0.00028795368,0.000741002,0.000020669997,0.0004018612,0.000022859604,0.00044434064,0.00010218048,0.001149536],"category_scores_gemma":[0.000035985202,0.00013425673,0.0003754865,0.00008491033,0.0058044665,0.00003315211,0.00028049116,0.00053793297,0.000003628234],"study_design_candidate":"design_other","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":[0.0017978892,0.0000864226,0.0506232,0.00019111906,0.0029348012,0.0000129145155,0.0015673833,0.0028338963,0.00003147003,0.13446982,0.018816717,0.7866344],"study_design_scores_gemma":[0.0014112646,0.0012661803,0.04645277,0.000030089923,0.00096309575,0.000020050498,0.00092406786,0.018640483,0.0000064203546,0.39129266,0.5382072,0.00078570604],"about_ca_topic_score_codex":0.010448727,"about_ca_topic_score_gemma":0.0013156774,"teacher_disagreement_score":0.7858487,"about_ca_system_score_codex":0.0000057366583,"about_ca_system_score_gemma":0.000043420692,"threshold_uncertainty_score":0.99976355},"labels":[],"label_agreement":null},{"id":"W4313322360","doi":"10.1130/2022.1220(04)","title":"Paleoproterozoic Earth and the transition toward modern tectonic processes: A synopsis","year":2022,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":false,"ca_institutions":"Acadia University; Geological Survey of Canada","funders":"","keywords":"Geology; Lithosphere; Subduction; Plate tectonics; Convergent boundary; Craton; Oceanic crust; Laurentia; Paleontology; Tectonics; Earth science","score_opus":0.014311431426949142,"score_gpt":0.17831976476222017,"score_spread":0.16400833333527104,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4313322360","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.02466547,0.010381699,0.001250279,0.0068797288,0.00007943982,0.0014925004,0.0004956472,0.00022434647,0.9545309],"genre_scores_gemma":[0.95758754,0.0029707039,0.0018354495,0.004511373,0.0001143193,0.00003500917,0.00028911297,0.000010813608,0.032645684],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9978978,0.000088160356,0.00046772684,0.0006293474,0.0005284795,0.00038851186],"domain_scores_gemma":[0.99868983,0.0004910973,0.00034283008,0.00024952085,0.00008689576,0.00013984797],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00028069533,0.0003918983,0.00088041235,0.000028305794,0.00032046568,0.000030293751,0.00041024204,0.00029190097,0.019279653],"category_scores_gemma":[0.00004328226,0.00021697186,0.00068678736,0.000079628844,0.0024965203,0.000034881778,0.000105244144,0.00077514147,0.000029322384],"study_design_candidate":"design_other","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":[0.0025456275,0.00019324035,0.0040591825,0.002233723,0.0035313424,0.000085423926,0.011666225,0.0038821318,0.0001708558,0.007905317,0.0014309549,0.96229595],"study_design_scores_gemma":[0.002692108,0.002294319,0.0040998124,0.00015806912,0.0014409763,0.00010348764,0.001333863,0.022451973,0.00008808424,0.80288756,0.16057467,0.0018750898],"about_ca_topic_score_codex":0.0011255569,"about_ca_topic_score_gemma":0.00008484886,"teacher_disagreement_score":0.9604209,"about_ca_system_score_codex":0.0000043855916,"about_ca_system_score_gemma":0.000051376905,"threshold_uncertainty_score":0.98161685},"labels":[],"label_agreement":null},{"id":"W4313322381","doi":"10.1130/2022.1220(19)","title":"Neoproterozoic of Laurentia","year":2022,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":28,"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":"Laurentia; Rodinia; Geology; Baltica; Paleontology; Supercontinent; Large igneous province; Paleomagnetism; Rift; Igneous rock; Terrane; Craton; Tectonics; Ordovician; Magmatism","score_opus":0.014913662334136242,"score_gpt":0.18413639202866652,"score_spread":0.16922272969453028,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4313322381","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0073973807,0.0012718176,0.00006878536,0.0003151394,0.00007769212,0.00024265627,0.0003319835,0.00005866199,0.99023587],"genre_scores_gemma":[0.61070985,0.000985899,0.012308931,0.0034583828,0.00026437177,0.0000114025415,0.0015081951,0.000022070122,0.3707309],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99787706,0.000044599594,0.00062539085,0.00051454536,0.0005798709,0.00035854452],"domain_scores_gemma":[0.99857503,0.00022622924,0.00063729356,0.0003288962,0.00008331588,0.00014920784],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00015940912,0.00034552428,0.0009764331,0.000038212373,0.00012032894,0.000006705633,0.00056122785,0.0003285141,0.19107795],"category_scores_gemma":[0.000021816491,0.00024503432,0.0012505325,0.000059015278,0.0013624919,0.000020215048,0.00017209954,0.0006378291,0.00009327322],"study_design_candidate":"design_other","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":[0.00054536853,0.00027494237,0.060971506,0.00078525505,0.0030257034,0.000075604294,0.00078029145,0.0019447561,0.000937959,0.021364272,0.023488203,0.88580614],"study_design_scores_gemma":[0.0004238341,0.0021256655,0.008730372,0.000052530882,0.00047137486,0.00001354887,0.00019433054,0.000833543,0.00023003062,0.23630968,0.7496994,0.0009156997],"about_ca_topic_score_codex":0.0016169543,"about_ca_topic_score_gemma":0.000038724276,"teacher_disagreement_score":0.88489044,"about_ca_system_score_codex":0.0000050193266,"about_ca_system_score_gemma":0.000033484423,"threshold_uncertainty_score":0.99922097},"labels":[],"label_agreement":null},{"id":"W4313322383","doi":"10.1130/2022.1220(16)","title":"Slow cooling in the metamorphic cores of Grenvillian large metamorphic core complexes and the thermal signature of the Ottawan orogenic lid","year":2022,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Geology; Hornblende; Metamorphic rock; Metamorphic core complex; Geochemistry; Gneiss; Geothermobarometry; Granulite; Metamorphism; Mafic; Mantle (geology); Biotite; Petrology; Metamorphic facies; Tectonics; Quartz; Facies; Geomorphology; Seismology; Extensional definition; Paleontology","score_opus":0.019779364165695763,"score_gpt":0.19382274711352712,"score_spread":0.17404338294783137,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4313322383","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8407851,0.020224698,0.00002520255,0.004703178,0.00014710794,0.0017226795,0.0012503399,0.000045900506,0.13109578],"genre_scores_gemma":[0.99417114,0.00053945207,0.00025855986,0.0022547836,0.0000483694,0.0000077743325,0.00011528785,0.000006424425,0.0025982324],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9971323,0.00038297713,0.00079661165,0.00046937366,0.0007919555,0.0004267877],"domain_scores_gemma":[0.9967299,0.0016580803,0.00094520295,0.0005064146,0.00008897644,0.000071404465],"candidate_categories":["sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011083814,0.0004124253,0.0012954872,0.000034759807,0.00033012417,0.000014397415,0.0013075505,0.00032480166,0.007882674],"category_scores_gemma":[0.00010776471,0.00016461799,0.0013733117,0.00017947535,0.0048609124,0.000023800458,0.00032624687,0.0013203018,0.0000037922812],"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":[0.004827307,0.0009830976,0.61526024,0.0016753953,0.012600767,0.00013124135,0.02483621,0.0149570685,0.004955309,0.22561465,0.0062922826,0.087866426],"study_design_scores_gemma":[0.005335474,0.0023015994,0.49505606,0.00029332712,0.0045202975,0.0001081208,0.008161058,0.013265213,0.00059015397,0.34638342,0.121837154,0.0021481195],"about_ca_topic_score_codex":0.0019907947,"about_ca_topic_score_gemma":0.00035568574,"teacher_disagreement_score":0.15338601,"about_ca_system_score_codex":0.0000045116,"about_ca_system_score_gemma":0.00004371236,"threshold_uncertainty_score":0.99784726},"labels":[],"label_agreement":null},{"id":"W4313322390","doi":"10.1130/2022.1220(07)","title":"A tectonic context for fluctuations in late Paleoproterozoic oxygen content","year":2022,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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 Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Proterozoic; Supercontinent; Geology; Plate tectonics; Earth science; Archean; Phanerozoic; Tectonics; Paleontology; Precambrian; Context (archaeology); Craton; Structural basin","score_opus":0.034638606942988044,"score_gpt":0.20722282247235946,"score_spread":0.17258421552937142,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4313322390","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.095277086,0.0043628593,0.00071352423,0.004221578,0.00023854748,0.0033111582,0.0017732399,0.00021994331,0.8898821],"genre_scores_gemma":[0.8357869,0.0005525839,0.004934861,0.00517686,0.00011848603,0.000108788205,0.0012050809,0.000015397176,0.15210108],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99775153,0.00004764887,0.00068561645,0.0006461039,0.00037090149,0.00049821736],"domain_scores_gemma":[0.99854136,0.00051979726,0.00042282062,0.0002665084,0.00009976857,0.00014974643],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00024978048,0.00037697438,0.0009550204,0.000057761426,0.00018781271,0.000014711077,0.00045086243,0.0003356475,0.0392735],"category_scores_gemma":[0.00006724669,0.00027538132,0.0010710639,0.00006766641,0.0008027965,0.000026197817,0.00010389747,0.0006177089,0.0000691003],"study_design_candidate":"design_other","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":[0.0010130752,0.00030343444,0.03796682,0.0005267503,0.0021984754,0.000060477476,0.001875531,0.0066390736,0.00097199465,0.017003404,0.0045360993,0.92690486],"study_design_scores_gemma":[0.0018937633,0.0027230256,0.05224469,0.00010063804,0.0004026885,0.000008126872,0.000731258,0.011134099,0.0000679344,0.38616946,0.5429732,0.0015510896],"about_ca_topic_score_codex":0.0025146904,"about_ca_topic_score_gemma":0.00059499126,"teacher_disagreement_score":0.92535377,"about_ca_system_score_codex":0.00001838128,"about_ca_system_score_gemma":0.000051875555,"threshold_uncertainty_score":0.99996984},"labels":[],"label_agreement":null},{"id":"W4313322392","doi":"10.1130/2022.1220(14)","title":"The late Mesoproterozoic to early Neoproterozoic Grenvillian orogeny and the assembly of Rodinia: Turning point in the tectonic evolution of Laurentia","year":2022,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Laurentia; Geology; Rodinia; Orogeny; Supercontinent; Proterozoic; Subduction; Geochemistry; Earth science; Paleontology; Magmatism; Craton; Ordovician; Tectonics","score_opus":0.009249569022047497,"score_gpt":0.18470290055375982,"score_spread":0.17545333153171233,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4313322392","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9148365,0.006220171,0.00018428042,0.0052541043,0.000089190835,0.0017730154,0.00014423157,0.00003487872,0.07146358],"genre_scores_gemma":[0.9954673,0.00028626135,0.0003263858,0.000548014,0.00003266826,0.000021988037,0.000026014035,0.0000049874716,0.0032863521],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9975644,0.0002861084,0.0007344198,0.00039543654,0.00062292727,0.00039675852],"domain_scores_gemma":[0.997815,0.0009490574,0.00067013985,0.00040889907,0.000077877055,0.000079022575],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011491312,0.0003133754,0.0007902785,0.000040052953,0.00031470403,0.0000244882,0.0008523461,0.0002190169,0.0016146284],"category_scores_gemma":[0.00010009796,0.0001348615,0.0006710955,0.00015659288,0.002102483,0.000027269865,0.00024260813,0.00082883093,0.000009746313],"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":[0.0062462,0.0004608304,0.25337154,0.0010297861,0.005641342,0.00007422423,0.03231593,0.014665431,0.0050176447,0.06482323,0.002979297,0.61337453],"study_design_scores_gemma":[0.0031318443,0.006441265,0.48523098,0.00033027932,0.0013086693,0.00005650453,0.00540636,0.006315301,0.0004491398,0.4351928,0.054462783,0.0016740819],"about_ca_topic_score_codex":0.0064160456,"about_ca_topic_score_gemma":0.0004930135,"teacher_disagreement_score":0.6117005,"about_ca_system_score_codex":0.000011504263,"about_ca_system_score_gemma":0.00003379256,"threshold_uncertainty_score":0.99929804},"labels":[],"label_agreement":null},{"id":"W4322632524","doi":"10.1130/spe560","title":"Geology of a Large Intact Extensional Oceanic Arc Crustal Section with Superior Exposures: Cretaceous Alisitos Arc, Baja California (Mexico)","year":2023,"lang":"en","type":"book","venue":"Geological Society of America eBooks","topic":"Geological and Tectonic Studies in Latin America","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 Victoria","funders":"University of California, Davis; National Science Foundation","keywords":"Geology; Caldera; Outcrop; Pluton; Cretaceous; Plutonism; Volcano; Sill; Silicic; Back-arc basin; Volcanic arc; Paleontology; Tectonics; Seismology; Geochemistry; Subduction","score_opus":0.013568809068657213,"score_gpt":0.21442832611445928,"score_spread":0.20085951704580207,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4322632524","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.09032698,0.0031243963,0.002496691,0.00074334466,0.0011257846,0.0020652462,0.0030119468,0.0007949559,0.8963106],"genre_scores_gemma":[0.8767572,0.0015316668,0.010653931,0.0036877536,0.00085285364,0.000042507294,0.0016571572,0.0000726233,0.10474429],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9955062,0.0002486092,0.0010621748,0.0011018404,0.000960924,0.0011202344],"domain_scores_gemma":[0.9965061,0.0014480464,0.0009586413,0.00053212367,0.00028622148,0.00026885653],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0004119991,0.00076975074,0.001894837,0.000098100056,0.0003920261,0.000017769977,0.0006694139,0.0008917399,0.010197053],"category_scores_gemma":[0.00020240659,0.00050695107,0.0009436572,0.00024736728,0.004053141,0.000040136827,0.00034511843,0.0012800343,0.00016268148],"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":[0.0072540734,0.0015147985,0.43794698,0.003003564,0.010996447,0.0014623539,0.0066343155,0.00664464,0.00070851954,0.0021598248,0.23142569,0.2902488],"study_design_scores_gemma":[0.005417624,0.026581291,0.41162956,0.0007600262,0.0011701308,0.00083943986,0.00709802,0.01049959,0.00014171812,0.022153592,0.5092404,0.004468643],"about_ca_topic_score_codex":0.000615582,"about_ca_topic_score_gemma":0.00005322608,"teacher_disagreement_score":0.7915664,"about_ca_system_score_codex":0.000037956524,"about_ca_system_score_gemma":0.00033654628,"threshold_uncertainty_score":0.9997382},"labels":[],"label_agreement":null},{"id":"W4322632525","doi":"10.1130/2023.2560(01)","title":"Geology of a Large Intact Extensional Oceanic Arc Crustal Section with Superior Exposures: Cretaceous Alisitos Arc, Baja California (Mexico)","year":2023,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Geology; Pluton; Rhyolite; Volcanic rock; Cretaceous; Caldera; Geochemistry; Subaerial; Unconformity; Volcanic arc; Paleontology; Volcano; Sedimentary rock; Subduction; Tectonics","score_opus":0.013314543402645523,"score_gpt":0.1966082361790336,"score_spread":0.1832936927763881,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4322632525","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5392094,0.0019343139,0.0016158855,0.001583865,0.00044328257,0.0015011084,0.0039217724,0.00062949874,0.44916084],"genre_scores_gemma":[0.95194334,0.00052494276,0.0028826075,0.0020125294,0.00032063096,0.000008799382,0.0014614328,0.000029210105,0.040816486],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9962658,0.0001106389,0.00094767543,0.0009899561,0.0008555019,0.0008303985],"domain_scores_gemma":[0.99759763,0.0006544501,0.0006979927,0.00042845285,0.00029463795,0.00032683893],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00031912158,0.0006643594,0.0016051064,0.00010034269,0.00023547756,0.000018593091,0.00051527424,0.0008935304,0.014666816],"category_scores_gemma":[0.000092845774,0.0004298935,0.0011821063,0.00014436469,0.0020575328,0.00004135266,0.00020462241,0.0010338043,0.00021449961],"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":[0.00897124,0.0014305261,0.80293226,0.002350889,0.013372825,0.001772377,0.0032635194,0.008500561,0.0074500497,0.013630615,0.029796313,0.10652885],"study_design_scores_gemma":[0.0067466525,0.024072375,0.32656428,0.0008998705,0.003342427,0.0009563723,0.0049407897,0.02722563,0.0017943553,0.2815955,0.3144984,0.0073633287],"about_ca_topic_score_codex":0.0013244093,"about_ca_topic_score_gemma":0.00026342322,"teacher_disagreement_score":0.47636795,"about_ca_system_score_codex":0.000014696018,"about_ca_system_score_gemma":0.00011376295,"threshold_uncertainty_score":0.9998153},"labels":[],"label_agreement":null},{"id":"W4377710212","doi":"10.1130/2023.0065(01)","title":"Geology and paleontology of Cretaceous and Paleocene sediments of the Cabin Branch, Cabin Creek (Cappy Avenue), and Tinkers Creek outcrops, Prince George’s County, Maryland","year":2023,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geology and Paleoclimatology Research","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; Outcrop; Cretaceous; Paleontology; Sedimentary depositional environment; Macrofossil; Glauconite; Biostratigraphy; Lithology; Lithostratigraphy; Sedimentary rock; Structural basin","score_opus":0.018590343768446413,"score_gpt":0.21921500454873782,"score_spread":0.2006246607802914,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4377710212","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9281924,0.0068245227,0.000018366401,0.0011819144,0.00021258018,0.00084662763,0.0005476013,0.000041322382,0.062134713],"genre_scores_gemma":[0.93355125,0.00685849,0.0008662468,0.00081511703,0.00005696429,0.00000909912,0.00013483813,0.000021185133,0.05768681],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99739623,0.0002488223,0.00068713794,0.0006950755,0.00036244444,0.0006102723],"domain_scores_gemma":[0.9973835,0.0012099969,0.00071308896,0.00038176175,0.00013268854,0.00017898975],"candidate_categories":["metaepi_narrow","sts"],"consensus_categories":[],"category_scores_codex":[0.0005613052,0.0003852892,0.0012732493,0.000056110974,0.0002580181,0.000012754296,0.00040767182,0.0009604448,0.0004900867],"category_scores_gemma":[0.00009916127,0.0003072334,0.0002262239,0.000055959063,0.009261976,0.000028242343,0.00030698167,0.00083408575,0.0000075743137],"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":[0.00013978707,0.000014526293,0.99085945,0.0003815044,0.00029596948,0.00002502936,0.0003834477,0.000009584182,0.000023014567,0.0001685835,0.00043882514,0.0072602774],"study_design_scores_gemma":[0.0009714866,0.00087768363,0.9779461,0.0001061411,0.0001726577,0.0002614001,0.00025712533,0.00023928467,0.000012657989,0.010131329,0.008659269,0.00036485362],"about_ca_topic_score_codex":0.0031547197,"about_ca_topic_score_gemma":0.0064344984,"teacher_disagreement_score":0.01291334,"about_ca_system_score_codex":0.0000025780498,"about_ca_system_score_gemma":0.00010089083,"threshold_uncertainty_score":0.99993795},"labels":[],"label_agreement":null},{"id":"W4388115261","doi":"10.1130/2023.0066(02)","title":"Geologic setting and organic architecture of Fallingwater, Frank Lloyd Wright’s masterpiece","year":2023,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Groundwater and Watershed Analysis","field":"Environmental Science","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":"","keywords":"Geology; Pennsylvanian; Fluvial; Syncline; Bedrock; Monocline; Paleontology; Geomorphology; Arenite; Alluvial fan; Mountain formation; Clastic rock; Tectonics; Structural basin","score_opus":0.011153818842412226,"score_gpt":0.18863492299105025,"score_spread":0.17748110414863802,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388115261","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.19587353,0.0007693489,0.023299402,0.0026258964,0.0003767094,0.00190529,0.00022244811,0.0010969485,0.7738304],"genre_scores_gemma":[0.49726674,0.00082275,0.018299647,0.001781241,0.00014919051,0.00002254797,0.00012204829,0.00013351256,0.4814023],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9975349,0.00005228527,0.0006484111,0.0007679812,0.0004955821,0.0005008883],"domain_scores_gemma":[0.99876624,0.0001702493,0.00050021283,0.00039349782,0.000025345276,0.00014447677],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00026380265,0.00049468904,0.00096435,0.000045130855,0.00014879697,0.000018598505,0.00046757367,0.000546284,0.0019272263],"category_scores_gemma":[0.000013730983,0.00034564117,0.0006204117,0.00006014537,0.002284289,0.000029122304,0.0009602584,0.00058710197,0.00014859503],"study_design_candidate":"design_other","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":[0.00057083723,0.000567605,0.109040104,0.0027990427,0.007506704,0.00036278088,0.0347764,0.0046099955,0.13285777,0.0040152585,0.02806075,0.67483276],"study_design_scores_gemma":[0.0049903695,0.0068048253,0.037192304,0.0014901664,0.0044141496,0.00026151858,0.0039486387,0.008269569,0.011050189,0.47898388,0.43310466,0.009489731],"about_ca_topic_score_codex":0.00031575296,"about_ca_topic_score_gemma":0.000009669151,"teacher_disagreement_score":0.66534305,"about_ca_system_score_codex":0.000048123213,"about_ca_system_score_gemma":0.000009818131,"threshold_uncertainty_score":0.99989957},"labels":[],"label_agreement":null},{"id":"W4395685423","doi":"10.1130/2024.0067(02)","title":"Big slow-movers, debris slides and flows, and mega-boulders of the Blue Ridge Escarpment, western North Carolina, USA","year":2024,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Landslides and related hazards","field":"Environmental Science","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":"BGC Engineering (Canada)","funders":"","keywords":"Landslide; Geology; Escarpment; Debris; Rockslide; Mass wasting; Rockfall; Ridge; Landform; Geomorphology; Debris flow; Physical geography; Geography; Paleontology; Oceanography","score_opus":0.010887134082216324,"score_gpt":0.19818901941996403,"score_spread":0.18730188533774772,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4395685423","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.73122394,0.0024390595,0.00008381869,0.00094784616,0.0003716636,0.0008239233,0.0002826087,0.00007278484,0.26375437],"genre_scores_gemma":[0.71875507,0.005404471,0.0012395312,0.0017192279,0.00013355137,0.000017011072,0.000025276837,0.00006885926,0.27263704],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99818987,0.000025571091,0.00042260124,0.00058935763,0.00043994724,0.00033266374],"domain_scores_gemma":[0.99910873,0.00009565034,0.0003111073,0.00032730857,0.000012602037,0.00014458611],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001203177,0.00039678192,0.00062041543,0.000017124534,0.00016420457,0.00002132521,0.0003108131,0.00047858985,0.00023045836],"category_scores_gemma":[0.0000075858557,0.00023122592,0.0004616692,0.000042034157,0.0025098023,0.000025078061,0.001003318,0.0006070624,0.000019368212],"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":[0.00034269624,0.0002317921,0.5507775,0.0013912843,0.0042019277,0.00010341841,0.0153404195,0.0014856998,0.002451937,0.0030859038,0.041196205,0.37939122],"study_design_scores_gemma":[0.0012399646,0.00093169557,0.13158031,0.00049296126,0.0012501486,0.00009373763,0.00059666595,0.0010210722,0.00039465114,0.0068474812,0.85411596,0.0014353514],"about_ca_topic_score_codex":0.00081576227,"about_ca_topic_score_gemma":0.00012720139,"teacher_disagreement_score":0.81291974,"about_ca_system_score_codex":0.00006472075,"about_ca_system_score_gemma":0.000022314225,"threshold_uncertainty_score":0.9429119},"labels":[],"label_agreement":null},{"id":"W4399163393","doi":"10.1130/2024.0069(01)","title":"Basement, belt, and batholith: Bedrock geology of the Idaho Panhandle","year":2024,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","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":"","keywords":"Geology; Supergroup; Basement; Batholith; Precambrian; Geochemistry; Gneiss; Metamorphic rock; Mafic; Clastic rock; Sedimentary rock; Paleontology; Archaeology; Tectonics; Geography","score_opus":0.013346210708295126,"score_gpt":0.18831878984982564,"score_spread":0.17497257914153053,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399163393","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.071518116,0.0046515726,0.000056772806,0.00130726,0.00014943608,0.0003401766,0.00034316897,0.0000631452,0.92157036],"genre_scores_gemma":[0.7387658,0.0010891702,0.0013495588,0.0017657808,0.00014305647,0.0000039407428,0.00014604142,0.000009961589,0.25672674],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99801534,0.00004330783,0.00057623634,0.00058937806,0.0003842414,0.0003915215],"domain_scores_gemma":[0.99870276,0.00033880773,0.0003880907,0.00033654724,0.00008493653,0.00014885134],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00018281283,0.00037991974,0.00087973214,0.000031143463,0.00013252159,0.000013033535,0.00044799445,0.00047253442,0.008792615],"category_scores_gemma":[0.00003502112,0.00020479751,0.00089051505,0.000065337226,0.0026520253,0.000016682245,0.00030309998,0.0006287839,0.00006416019],"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":[0.0005046954,0.0003252211,0.4153747,0.0027591465,0.0063058236,0.00013062816,0.002548805,0.0006950045,0.002253998,0.097716406,0.01870899,0.45267656],"study_design_scores_gemma":[0.00042074829,0.0011844658,0.04235844,0.00019497128,0.00090563984,0.00005629897,0.00030810852,0.0022237452,0.00050670234,0.7291629,0.22177576,0.0009022851],"about_ca_topic_score_codex":0.0019074053,"about_ca_topic_score_gemma":0.00014013743,"teacher_disagreement_score":0.66724765,"about_ca_system_score_codex":0.000004417179,"about_ca_system_score_gemma":0.000031505755,"threshold_uncertainty_score":0.9921135},"labels":[],"label_agreement":null},{"id":"W4405664223","doi":"10.1130/2025.2563(02)","title":"Geochemical transition from Miocene–Pliocene to Quaternary arc volcanism in the northern Sierra Nevada, California","year":2024,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa; Carleton University","funders":"","keywords":"Geology; Lava; Subduction; Volcanism; Geochemistry; Volcanic arc; Basalt; Volcanic rock; Quaternary; Island arc; Volcano; Late Miocene; Mantle (geology); Paleontology; Structural basin; Tectonics","score_opus":0.013823354210912643,"score_gpt":0.19126945088760902,"score_spread":0.1774460966766964,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405664223","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5644392,0.002767617,0.00044241236,0.013866168,0.00020228907,0.0009817673,0.003068448,0.00019864965,0.4140335],"genre_scores_gemma":[0.9696946,0.00026241312,0.002303099,0.011144944,0.00046669046,0.000014902556,0.0017112746,0.000018715114,0.014383366],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99689955,0.00006767987,0.0007542546,0.0009410985,0.0007259891,0.0006114376],"domain_scores_gemma":[0.9985747,0.00046490494,0.00020780331,0.0004074947,0.00007751979,0.00026759162],"candidate_categories":["metaepi_narrow","insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00024820695,0.0005722565,0.00095161103,0.000058797235,0.00011143705,0.000044879398,0.00079498405,0.00063369377,0.008457328],"category_scores_gemma":[0.000026081405,0.0003383477,0.0010173633,0.00012693895,0.00081200345,0.000024092771,0.0000993065,0.0010839652,0.0010354024],"study_design_candidate":"theoretical_or_conceptual","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":[0.0030584373,0.0011913893,0.1541627,0.0012357932,0.005650985,0.0022781284,0.023407185,0.013485296,0.0069261394,0.0043562683,0.04831295,0.73593473],"study_design_scores_gemma":[0.0007776802,0.0014065701,0.020753399,0.00039845356,0.00087091426,0.00004402875,0.0019100856,0.013869575,0.00038949342,0.796197,0.16123194,0.002150837],"about_ca_topic_score_codex":0.015395292,"about_ca_topic_score_gemma":0.0014057142,"teacher_disagreement_score":0.79184073,"about_ca_system_score_codex":0.000021517642,"about_ca_system_score_gemma":0.000043367214,"threshold_uncertainty_score":0.99990684},"labels":[],"label_agreement":null},{"id":"W4413013390","doi":"10.1130/2025.2565(05)","title":"Reconciling Baja–British Columbia and flat Shatsky conjugate subduction beneath the western United States","year":2025,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Tectonic Studies in Latin America","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":"Subduction; Geology; Seismology; Conjugate","score_opus":0.0159932487724245,"score_gpt":0.19763097717890388,"score_spread":0.18163772840647938,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413013390","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.03310116,0.0042062458,0.00017905812,0.0013502216,0.00045700953,0.00084341585,0.00056507095,0.00023503578,0.95906276],"genre_scores_gemma":[0.18230082,0.02343935,0.005861295,0.014639263,0.00039750087,0.000022088492,0.0011361791,0.000027820928,0.77217567],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9978599,0.00008270387,0.0005703619,0.00067379297,0.0003353923,0.00047783702],"domain_scores_gemma":[0.99799556,0.000992022,0.00045266587,0.0002928498,0.00015315771,0.00011374797],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00027753282,0.0003428136,0.0008258375,0.000021890419,0.0006266611,0.00013031068,0.0003826774,0.0004025278,0.0056145187],"category_scores_gemma":[0.00007052475,0.00028903186,0.0003664368,0.00007633333,0.0037032429,0.000030161644,0.00021132971,0.00072959694,0.000021627407],"study_design_candidate":"not_applicable","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":[0.00005211245,0.000013010702,0.03641279,0.00014339671,0.00058411265,0.000022301367,0.00045194948,0.0001735185,0.0000018871714,0.00015320718,0.02475149,0.93724024],"study_design_scores_gemma":[0.0005927405,0.0012654641,0.045032725,0.00032261998,0.0003084122,0.000066931214,0.0010287539,0.0039906604,0.0000028797863,0.022583814,0.92387116,0.000933864],"about_ca_topic_score_codex":0.023033503,"about_ca_topic_score_gemma":0.0017528686,"teacher_disagreement_score":0.93630636,"about_ca_system_score_codex":0.000012346438,"about_ca_system_score_gemma":0.00004307389,"threshold_uncertainty_score":0.9999562},"labels":[],"label_agreement":null},{"id":"W4414600423","doi":"10.1130/2025.2565(08)","title":"The Cretaceous–Paleogene Ross Lake fault system: Relationships between magmatism and faulting during large-scale translation in the northern North American Cordillera of Washington and British Columbia","year":2025,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","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":"","keywords":"Mylonite; Sinistral and dextral; Fault (geology); Fault scarp; Shear zone; Strike-slip tectonics; Metamorphic rock; Tectonics; Gneiss; Echelon formation","score_opus":0.011672618075247582,"score_gpt":0.18399851790521843,"score_spread":0.17232589982997085,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414600423","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9562829,0.0028337438,0.000072722236,0.0002967879,0.000015624897,0.00046870508,0.00049545505,0.00003639312,0.039497677],"genre_scores_gemma":[0.9945739,0.0009859087,0.0009964419,0.00008781381,0.000044815388,0.0000066296266,0.0002401595,0.000005263734,0.0030590896],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99782753,0.00019887977,0.0007288394,0.0004705624,0.00040108943,0.00037312208],"domain_scores_gemma":[0.9975669,0.0014435786,0.0005823074,0.0002188117,0.000095162824,0.00009325331],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004928095,0.0002417283,0.00079073344,0.000021536822,0.0006767134,0.000111373585,0.00032828574,0.00023567697,0.0001440478],"category_scores_gemma":[0.00007058956,0.00018252117,0.00029005122,0.00013278813,0.0014748668,0.00003422817,0.00007372742,0.0007476078,0.0000017030152],"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":[0.000019416795,0.000009466618,0.81447184,0.00014133607,0.00014290561,0.0000045915936,0.00067110645,0.00009833262,0.000002744874,0.0000049611294,0.00003223998,0.18440108],"study_design_scores_gemma":[0.0002923986,0.00014677318,0.98970914,0.0001534557,0.00022602611,0.000010250924,0.0020357582,0.002809166,0.0000016965092,0.0009194665,0.0034302366,0.00026561445],"about_ca_topic_score_codex":0.0076248525,"about_ca_topic_score_gemma":0.31189242,"teacher_disagreement_score":0.3042676,"about_ca_system_score_codex":0.0000063438615,"about_ca_system_score_gemma":0.00002168208,"threshold_uncertainty_score":0.99898344},"labels":[],"label_agreement":null},{"id":"W4415257736","doi":"10.1130/2025.2565(14)","title":"Late Cretaceous intra-arc transpression and thrusting in the Southern California batholith support moderate “Sierra–British Columbia” translation models","year":2025,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","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":"Mylonite; Sinistral and dextral; Transpression; Shear zone; Batholith; Overprinting; Cretaceous; Shear (geology)","score_opus":0.01959911529448838,"score_gpt":0.2056757840041664,"score_spread":0.186076668709678,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415257736","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.01640312,0.003464137,0.14265442,0.00069185375,0.00012031157,0.0015676407,0.0010565593,0.0005642628,0.8334777],"genre_scores_gemma":[0.9190886,0.0052679186,0.0053830226,0.0013354167,0.0001373761,0.00010882932,0.000396346,0.0001082771,0.068174236],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99831617,0.00006792556,0.00059509324,0.00037345142,0.00033418,0.00031320602],"domain_scores_gemma":[0.9994045,0.00012188303,0.00012575834,0.00021912807,0.000051868356,0.00007685839],"candidate_categories":["metaepi_narrow"],"consensus_categories":[],"category_scores_codex":[0.0002796731,0.00027987157,0.0006757838,0.000037199232,0.0001564665,0.00010882099,0.0002244577,0.000505324,0.00022224332],"category_scores_gemma":[0.000006277578,0.00027058533,0.00039105772,0.00005194837,0.00036467737,0.00004508149,0.000034537337,0.00073422637,0.0000038862104],"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":[0.000105497675,0.00010062468,0.00015055413,0.0014697876,0.0012012578,0.00012740222,0.03206071,0.5288389,0.00061080215,0.00025923838,0.0062939147,0.42878133],"study_design_scores_gemma":[0.00047824252,0.00007107265,0.000013599382,0.00025566647,0.00022205136,0.000009319467,0.0007328837,0.96781,0.00000894204,0.016710024,0.013238415,0.00044981367],"about_ca_topic_score_codex":0.00068449415,"about_ca_topic_score_gemma":0.0005348595,"teacher_disagreement_score":0.90268546,"about_ca_system_score_codex":0.000032084172,"about_ca_system_score_gemma":0.000034544315,"threshold_uncertainty_score":0.9999746},"labels":[],"label_agreement":null},{"id":"W4415526587","doi":"10.1130/2025.2565(09)","title":"Formation and extent of the Cretaceous West Mountains plutonic complex","year":2025,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological Studies and Exploration","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":"Cameco (Canada)","funders":"","keywords":"Pluton; Batholith; Zircon; Terrane; Magmatism; Back-arc basin; Cretaceous; Island arc","score_opus":0.02906538565894842,"score_gpt":0.2075396361825403,"score_spread":0.17847425052359187,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415526587","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0073546646,0.0033371896,0.00096511736,0.0027107203,0.00015958409,0.0008156744,0.00023414833,0.000056536413,0.98436636],"genre_scores_gemma":[0.892627,0.0052591166,0.0044860067,0.0039824797,0.00011349158,0.000007488156,0.00029243602,0.000007582338,0.09322439],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9988521,0.000033897708,0.000397376,0.0002416052,0.00026442116,0.00021064024],"domain_scores_gemma":[0.99911,0.00017064402,0.0004077096,0.00018095449,0.00008259013,0.000048130267],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.000115239265,0.00021242634,0.00047238922,0.000013567834,0.00023558467,0.000011729859,0.00022631229,0.00023064842,0.0010009452],"category_scores_gemma":[0.000021511627,0.000121279125,0.00031536582,0.000028215793,0.0011599074,0.000027467331,0.00013339303,0.00025380784,0.000012722496],"study_design_candidate":"design_other","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":[0.00019251922,0.000058687932,0.014041754,0.0006869591,0.0005656784,0.0000040810914,0.0022648799,0.0017448696,0.00010278411,0.020018522,0.019995598,0.94032365],"study_design_scores_gemma":[0.00059540634,0.0013948298,0.17972459,0.00021060165,0.00025967017,0.000014591015,0.0016574729,0.015104217,0.000034302364,0.057056915,0.7433085,0.00063893566],"about_ca_topic_score_codex":0.0003519261,"about_ca_topic_score_gemma":0.00010734599,"teacher_disagreement_score":0.93968475,"about_ca_system_score_codex":0.000008983231,"about_ca_system_score_gemma":0.000029211618,"threshold_uncertainty_score":0.99991226},"labels":[],"label_agreement":null},{"id":"W4415529241","doi":"10.1130/2025.0074(04)","title":"The West Texas nexus: Orogeny, magmatism, K-Pg boundary, vertebrate biostratigraphy, and Chihuahuan Desert geohydrology","year":2025,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Evolution and Paleontology 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":"","keywords":"Paleozoic; Cenozoic; Proterozoic; Geological survey; Magmatism; Cretaceous; Hydrogeology; Desert (philosophy); Kimberlite","score_opus":0.012973307643061378,"score_gpt":0.20973748709452975,"score_spread":0.19676417945146837,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415529241","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0018722982,0.02092139,0.00008570748,0.0029526586,0.00032241188,0.00043691407,0.00021996992,0.00010216396,0.9730865],"genre_scores_gemma":[0.30064052,0.0373645,0.008027374,0.022218822,0.00054818933,0.000027371914,0.0006258432,0.00004038229,0.630507],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9979792,0.00010976328,0.00053859607,0.00056560646,0.000260247,0.00054654595],"domain_scores_gemma":[0.99830294,0.00075102836,0.0003760846,0.00033805383,0.0000881644,0.0001437308],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002663216,0.00045767054,0.00076477806,0.00004615138,0.00088116474,0.00005255438,0.0004522554,0.0005800965,0.0009990638],"category_scores_gemma":[0.00003449149,0.0002927212,0.0004249839,0.000050336857,0.0061445376,0.000033805143,0.00010727592,0.00065157434,0.00007966502],"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":[0.00031282127,0.000045585424,0.37713107,0.00029499488,0.0029236136,0.000047607748,0.0012159732,0.000026444948,0.000010528377,0.042011816,0.09913496,0.47684458],"study_design_scores_gemma":[0.00046852566,0.0009622647,0.1830939,0.00007494806,0.00023462805,0.00004983683,0.00040968964,0.0015167587,0.0000039530164,0.05584262,0.7567217,0.0006211907],"about_ca_topic_score_codex":0.00084764126,"about_ca_topic_score_gemma":0.006696896,"teacher_disagreement_score":0.6575867,"about_ca_system_score_codex":0.0000054299253,"about_ca_system_score_gemma":0.0001237972,"threshold_uncertainty_score":0.9999525},"labels":[],"label_agreement":null},{"id":"W4415748513","doi":"10.1130/2025.2565(06)","title":"Geochemical constraints on the petrogenesis of Eocene volcanic rocks from the Terrace Mountain volcanic complex, south-central British Columbia: Tectonic implications","year":2025,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","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":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Saint Mary's University","funders":"","keywords":"Volcanic rock; Volcano; Petrogenesis; Mafic; Rhyolite; Basalt; Continental crust; Volcanic plateau; Trachyte","score_opus":0.017318745642686064,"score_gpt":0.1912656896603221,"score_spread":0.17394694401763602,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415748513","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.46266603,0.003471121,0.0011762768,0.010910715,0.00021169048,0.0023569902,0.014537226,0.00028632698,0.5043836],"genre_scores_gemma":[0.9803032,0.00030176356,0.00058208726,0.004474161,0.00013528985,0.000015854685,0.0008727468,0.0000094677835,0.013305382],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99677813,0.00013532653,0.0008965693,0.0008827517,0.00058469735,0.0007224973],"domain_scores_gemma":[0.9961769,0.0019628021,0.00073189446,0.00071803236,0.00019981629,0.00021053707],"candidate_categories":["metaepi_narrow","sts","insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00023638201,0.00045082043,0.001129155,0.000017476026,0.00048728826,0.00008709265,0.0013412454,0.0005723019,0.040532622],"category_scores_gemma":[0.00018390329,0.00032967312,0.0013984535,0.00014098203,0.004325859,0.000017868115,0.00024470058,0.0010057869,0.0000495565],"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":[0.0003459349,0.00041097886,0.39386585,0.00020993075,0.0059431046,0.00003088827,0.0007989887,0.00076523947,0.0018320471,0.0024080335,0.14616695,0.44722205],"study_design_scores_gemma":[0.001411673,0.0010980713,0.7491339,0.0004901049,0.0020463637,0.000046920642,0.0018888122,0.0037996215,0.0002645668,0.17263281,0.06517597,0.0020111916],"about_ca_topic_score_codex":0.036486693,"about_ca_topic_score_gemma":0.012305656,"teacher_disagreement_score":0.51763725,"about_ca_system_score_codex":0.000030982534,"about_ca_system_score_gemma":0.00016672835,"threshold_uncertainty_score":0.99991554},"labels":[],"label_agreement":null},{"id":"W4415748524","doi":"10.1130/2025.2565(07)","title":"Sinistral shear zones along the central and southern portions of coastal British Columbia, Canada","year":2025,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","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":"","keywords":"Sinistral and dextral; Cretaceous; Terrane; Shear zone; Shear (geology)","score_opus":0.007203502203674003,"score_gpt":0.1606334408170312,"score_spread":0.15342993861335721,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415748524","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.398364,0.0022179019,0.00015493036,0.0021095774,0.00017825942,0.00057629147,0.006390326,0.00006801716,0.5899407],"genre_scores_gemma":[0.84369814,0.00021848317,0.0007216753,0.0010856079,0.000061266575,0.0000014080282,0.000310442,0.0000033472068,0.15389964],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99831665,0.000035264624,0.0005147268,0.0003771292,0.0003700925,0.00038613428],"domain_scores_gemma":[0.99892426,0.00031314394,0.0003300936,0.0001767667,0.00009784349,0.00015791964],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00009860411,0.00020061956,0.00064572674,0.000007117664,0.00023156418,0.000040620103,0.0002905654,0.00024413066,0.007780899],"category_scores_gemma":[0.000037356105,0.00016912767,0.0004498718,0.00004152854,0.0017771755,0.000011802323,0.000094755465,0.0003892936,0.0000025973195],"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":[0.000053471307,0.00006218151,0.7598047,0.00022146378,0.0010838554,0.000070186645,0.00027440407,0.00029058984,0.000014144635,0.0006404649,0.023843894,0.2136406],"study_design_scores_gemma":[0.0005088294,0.00065847597,0.84537566,0.00023234435,0.0007437998,0.000066374734,0.0019282551,0.0016524042,0.000009033892,0.04762168,0.10016702,0.0010361336],"about_ca_topic_score_codex":0.96617234,"about_ca_topic_score_gemma":0.95081097,"teacher_disagreement_score":0.44533414,"about_ca_system_score_codex":0.000004987285,"about_ca_system_score_gemma":0.00021174196,"threshold_uncertainty_score":0.9931261},"labels":[],"label_agreement":null},{"id":"W4416660977","doi":"10.1130/2025.2565(02)","title":"New paleotemperature and paleobiological results consistent with a far-traveled alternative for the Baja-BC hypothesis","year":2025,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Paleontology and Stratigraphy of Fossils","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":"","keywords":"San Joaquin; Cretaceous; Phreatic; Ammonite; Structural basin; Sedimentary basin","score_opus":0.023934030330107017,"score_gpt":0.20893988532090313,"score_spread":0.1850058549907961,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416660977","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0006498884,0.014707785,0.0027488887,0.0029916482,0.00016728017,0.0016325124,0.0016324886,0.00008430065,0.9753852],"genre_scores_gemma":[0.3733751,0.012924356,0.16151397,0.009986315,0.0010725622,0.000091514325,0.00051280187,0.00002238553,0.440501],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99816364,0.0000682629,0.00045714248,0.00068042753,0.00023079322,0.00039973564],"domain_scores_gemma":[0.99605346,0.0029692696,0.0004257462,0.0002880815,0.00010528708,0.00015817946],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023605023,0.00046251342,0.00083287293,0.000029238952,0.00037192137,0.00003613916,0.00039847757,0.0006849906,0.00017607868],"category_scores_gemma":[0.00007768198,0.0002360398,0.0005364582,0.000032268308,0.0024223183,0.000020711685,0.000013178329,0.0006338556,0.0000021492026],"study_design_candidate":"design_other","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":[0.001924951,0.000016956077,0.005118408,0.00008731994,0.0016519973,0.00002055407,0.00059829146,0.000026516047,0.000010992495,0.00508886,0.012672166,0.97278297],"study_design_scores_gemma":[0.004521868,0.00717586,0.6002825,0.0004790697,0.001300811,0.00010239142,0.0013623699,0.0011782254,0.000060508555,0.058104135,0.32365638,0.0017758679],"about_ca_topic_score_codex":0.00038614933,"about_ca_topic_score_gemma":0.00045027104,"teacher_disagreement_score":0.9710071,"about_ca_system_score_codex":0.0000032661426,"about_ca_system_score_gemma":0.00013939597,"threshold_uncertainty_score":0.9625424},"labels":[],"label_agreement":null},{"id":"W7084115197","doi":"10.1130/2025.2565(15)","title":"Dating deformation in the Alamo Mountain and Piru Creek shear zones: Insights into Late Cretaceous tectonics in southern California","year":2025,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Seismic Performance and Analysis","field":"Engineering","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":"Sinistral and dextral; Terrane; Cretaceous; Shear zone; North American Plate; Mylonite; Mesozoic; Shear (geology); Zircon","score_opus":0.008277416707747868,"score_gpt":0.19776593427015896,"score_spread":0.18948851756241109,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7084115197","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6656251,0.006286101,0.012020137,0.0005145244,0.00009087732,0.0012320707,0.00012521811,0.00038098238,0.313725],"genre_scores_gemma":[0.9597891,0.005650593,0.007494868,0.004355305,0.00015335984,0.000111152585,0.0003150734,0.00009173132,0.022038832],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9987252,0.000030152487,0.00053336844,0.00023908884,0.00021474187,0.00025745764],"domain_scores_gemma":[0.99943507,0.00013457617,0.00014079687,0.00022699097,0.000029332847,0.00003321516],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022956617,0.00027769443,0.0005361263,0.00008502788,0.00008848009,0.000030958832,0.00023979593,0.00035228112,0.00004613551],"category_scores_gemma":[0.0000144251435,0.00020725989,0.00019568719,0.000084476414,0.00027762944,0.00004018461,0.00010660765,0.0006794689,0.000015623373],"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":[0.00011546328,0.00013504465,0.006772965,0.0031079503,0.0014451678,0.000084682404,0.11440704,0.11266426,0.00069600815,0.0016142562,0.003878629,0.75507855],"study_design_scores_gemma":[0.00080451486,0.0001874745,0.0004770516,0.00066627807,0.00019057718,0.000008641103,0.0139311105,0.85309714,0.000025173938,0.016875887,0.112803616,0.00093254016],"about_ca_topic_score_codex":0.00068613864,"about_ca_topic_score_gemma":0.00012497487,"teacher_disagreement_score":0.754146,"about_ca_system_score_codex":0.00009421703,"about_ca_system_score_gemma":0.000026485604,"threshold_uncertainty_score":0.84518135},"labels":[],"label_agreement":null},{"id":"W74600674","doi":"10.1130/dnag-gna-d2.25","title":"Tectonic evolution of the craton in Phanerozoic time","year":2015,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":156,"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":"Craton; Geology; Phanerozoic; Tectonics; Proterozoic; Paleontology; Unconformity; Plate tectonics; Earth science; Cenozoic; Structural basin","score_opus":0.015442863341965974,"score_gpt":0.18702852044116303,"score_spread":0.17158565709919704,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W74600674","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"codex-gemma-dda1882f352a","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.04372062,0.0025256628,0.00003501416,0.0005053204,0.000065547894,0.00032830582,0.00012543744,0.000041507166,0.9526526],"genre_scores_gemma":[0.887286,0.0000934784,0.00066354993,0.00038206094,0.00007055041,0.0000019589213,0.00007347721,0.0000053948706,0.11142349],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9981388,0.00006679952,0.0005481382,0.00040386475,0.00050858065,0.0003338132],"domain_scores_gemma":[0.9987815,0.00019043074,0.0004807953,0.00031526093,0.00012235285,0.000109630324],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00026888144,0.00028805822,0.0007775484,0.000034968016,0.00005725074,0.0000050459107,0.0005400973,0.0004569891,0.011137466],"category_scores_gemma":[0.000058100224,0.00016039702,0.0007389022,0.00010645275,0.0015409248,0.00001918436,0.00012000266,0.00054007827,0.00015890776],"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":[0.001017479,0.0006486476,0.34277987,0.0008525866,0.0023057656,0.00005210503,0.0014518753,0.015859796,0.0071503813,0.016278312,0.04063927,0.5709639],"study_design_scores_gemma":[0.0011090804,0.0016020741,0.11236224,0.0002997066,0.00046447245,0.000019730902,0.0002528356,0.01195113,0.00051612617,0.7617035,0.10836566,0.0013534235],"about_ca_topic_score_codex":0.0020954001,"about_ca_topic_score_gemma":0.00015397272,"teacher_disagreement_score":0.8435654,"about_ca_system_score_codex":0.000023533756,"about_ca_system_score_gemma":0.00008656793,"threshold_uncertainty_score":0.9897665},"labels":[],"label_agreement":null}]}